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Avalanches: forest interactions and risk management Frank Krumm 1 and Peter Bebi 1,2 1. WSL-Institute for Snow and Avalanche Research, SLF 2. Swiss Federal Institute for Forest, Snow and Landscape Research

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Page 1: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Overview

1 Avalanche protection The role of mounain forests

2 History of Avalanche Protection 3 Interactions with other natural hazards 4 Avalanche-forest interactions in a warmer

Climate 5 Conclusions

Avalanche protection ndash The role of mountain forests

Main effect Avalanche releases do generally not occur in closed forested terrain

Small avalanches may be stopped in the forest (detrainment of snow behind trees)

More irregular snow cover around trees and in forests and decrease of snow depth

Source H Imbeck (1987)

Avalanche protection ndash The role of mountain forests

Amount and duration of incoming

solar radiation are reduced in the

forest

Outgoing long-wave radiation

reduced

Avalanche protection ndash The role of mountain forests

Surface hoar is less

probable in forests

Reduction of wind speeds in the forest compared to open

areas and large gaps

Wind-transport

Source M Frehner

(from Meyer 1987 and

Cemagref)

Avalanche protection ndash The role of mountain forests

Terrain roughness of

standing and laying

stems

But critical stem densities

would be very high only with

this effect ~ 500 stems 30o

~ 1000 stems 40o (Saeki amp Matsuoka 1970 Salm 1978)

Avalanche protection ndash The role of mountain forests

Relationship between critical gap widths and crown cover densities for triggering of

avalanches for different categories of slope steepness Source Schneebeli und Bebi 2004

Crown cover ()

Avalanche protection ndash The role of mountain forests

Limits of avalache protection

Large avalanches from above the treeline can generally not be stopped by the forest

New tols for regional scale avalanche hazard mapping

Avalanche dynamic model

(RAMMS) Newly available remote sensing data

-gtImproved decicion support for management of protection forests

Evaluating protective effects against avalanches

GIS-based risk analysis R = AS P

Probability of avalanche releases Developing forest cover scenarios

bull Comparison of risks depending on forest cover scenarios

bull Determination of the value of the forest for avalanche protection (up to 150rsquo000 Euro ha and year in this case study

Mapping of forest structures

Simulating avalanche

runout

Risk calculation

R = AS P

Historic view on snow avalanche catastrophies

218 BC Hannibal crossing the Alps Loss of ca 18rsquo000 peoble by avalanches

Guides caught by avalanches at Gd St Bernard as they started while pilgrims were praying (Rudolf de St Trout 1228 )

Trento December 13th 1916 (White Friday) Ca 9000 killed people

18 Jan 2017 Rigopiano Abruzzo 19 people death

History of avalanche protection Example Andermatt

Situation in the beginning of 19th

century bdquoOnly few old trees are standing in the

forest they look sadly down - like Noah

once did with his sons from the mountain

Ararat (Kasthofer 1822)raquo

How effective was the Bannbrief

Early deforestation and overview of

the valley (c 10th-14th century)

Bannbrief (written order) 1397 Any

use of forest product in remaining

forest is not allowed

Bildvergleich bis 2009

Geschichte des Bannwaldes

Photos Photoarchiv Xaver Buumlhlmann Andermatt

Increase of settlement and

infrastructure in the 20th

century

Increased afforestation and

forest density increasae of

forest area from 4 to 24 ha

Windthrow bdquoVivianldquo 1990

History of avalanche protection Example Andermatt

bull Increase of avalanche protection since the 19th century

bull Passive and

active afforestation

Davos ca 1940

Davos 2012

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 2: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Overview

1 Avalanche protection The role of mounain forests

2 History of Avalanche Protection 3 Interactions with other natural hazards 4 Avalanche-forest interactions in a warmer

Climate 5 Conclusions

Avalanche protection ndash The role of mountain forests

Main effect Avalanche releases do generally not occur in closed forested terrain

Small avalanches may be stopped in the forest (detrainment of snow behind trees)

More irregular snow cover around trees and in forests and decrease of snow depth

Source H Imbeck (1987)

Avalanche protection ndash The role of mountain forests

Amount and duration of incoming

solar radiation are reduced in the

forest

Outgoing long-wave radiation

reduced

Avalanche protection ndash The role of mountain forests

Surface hoar is less

probable in forests

Reduction of wind speeds in the forest compared to open

areas and large gaps

Wind-transport

Source M Frehner

(from Meyer 1987 and

Cemagref)

Avalanche protection ndash The role of mountain forests

Terrain roughness of

standing and laying

stems

But critical stem densities

would be very high only with

this effect ~ 500 stems 30o

~ 1000 stems 40o (Saeki amp Matsuoka 1970 Salm 1978)

Avalanche protection ndash The role of mountain forests

Relationship between critical gap widths and crown cover densities for triggering of

avalanches for different categories of slope steepness Source Schneebeli und Bebi 2004

Crown cover ()

Avalanche protection ndash The role of mountain forests

Limits of avalache protection

Large avalanches from above the treeline can generally not be stopped by the forest

New tols for regional scale avalanche hazard mapping

Avalanche dynamic model

(RAMMS) Newly available remote sensing data

-gtImproved decicion support for management of protection forests

Evaluating protective effects against avalanches

GIS-based risk analysis R = AS P

Probability of avalanche releases Developing forest cover scenarios

bull Comparison of risks depending on forest cover scenarios

bull Determination of the value of the forest for avalanche protection (up to 150rsquo000 Euro ha and year in this case study

Mapping of forest structures

Simulating avalanche

runout

Risk calculation

R = AS P

Historic view on snow avalanche catastrophies

218 BC Hannibal crossing the Alps Loss of ca 18rsquo000 peoble by avalanches

Guides caught by avalanches at Gd St Bernard as they started while pilgrims were praying (Rudolf de St Trout 1228 )

Trento December 13th 1916 (White Friday) Ca 9000 killed people

18 Jan 2017 Rigopiano Abruzzo 19 people death

History of avalanche protection Example Andermatt

Situation in the beginning of 19th

century bdquoOnly few old trees are standing in the

forest they look sadly down - like Noah

once did with his sons from the mountain

Ararat (Kasthofer 1822)raquo

How effective was the Bannbrief

Early deforestation and overview of

the valley (c 10th-14th century)

Bannbrief (written order) 1397 Any

use of forest product in remaining

forest is not allowed

Bildvergleich bis 2009

Geschichte des Bannwaldes

Photos Photoarchiv Xaver Buumlhlmann Andermatt

Increase of settlement and

infrastructure in the 20th

century

Increased afforestation and

forest density increasae of

forest area from 4 to 24 ha

Windthrow bdquoVivianldquo 1990

History of avalanche protection Example Andermatt

bull Increase of avalanche protection since the 19th century

bull Passive and

active afforestation

Davos ca 1940

Davos 2012

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 3: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Avalanche protection ndash The role of mountain forests

Main effect Avalanche releases do generally not occur in closed forested terrain

Small avalanches may be stopped in the forest (detrainment of snow behind trees)

More irregular snow cover around trees and in forests and decrease of snow depth

Source H Imbeck (1987)

Avalanche protection ndash The role of mountain forests

Amount and duration of incoming

solar radiation are reduced in the

forest

Outgoing long-wave radiation

reduced

Avalanche protection ndash The role of mountain forests

Surface hoar is less

probable in forests

Reduction of wind speeds in the forest compared to open

areas and large gaps

Wind-transport

Source M Frehner

(from Meyer 1987 and

Cemagref)

Avalanche protection ndash The role of mountain forests

Terrain roughness of

standing and laying

stems

But critical stem densities

would be very high only with

this effect ~ 500 stems 30o

~ 1000 stems 40o (Saeki amp Matsuoka 1970 Salm 1978)

Avalanche protection ndash The role of mountain forests

Relationship between critical gap widths and crown cover densities for triggering of

avalanches for different categories of slope steepness Source Schneebeli und Bebi 2004

Crown cover ()

Avalanche protection ndash The role of mountain forests

Limits of avalache protection

Large avalanches from above the treeline can generally not be stopped by the forest

New tols for regional scale avalanche hazard mapping

Avalanche dynamic model

(RAMMS) Newly available remote sensing data

-gtImproved decicion support for management of protection forests

Evaluating protective effects against avalanches

GIS-based risk analysis R = AS P

Probability of avalanche releases Developing forest cover scenarios

bull Comparison of risks depending on forest cover scenarios

bull Determination of the value of the forest for avalanche protection (up to 150rsquo000 Euro ha and year in this case study

Mapping of forest structures

Simulating avalanche

runout

Risk calculation

R = AS P

Historic view on snow avalanche catastrophies

218 BC Hannibal crossing the Alps Loss of ca 18rsquo000 peoble by avalanches

Guides caught by avalanches at Gd St Bernard as they started while pilgrims were praying (Rudolf de St Trout 1228 )

Trento December 13th 1916 (White Friday) Ca 9000 killed people

18 Jan 2017 Rigopiano Abruzzo 19 people death

History of avalanche protection Example Andermatt

Situation in the beginning of 19th

century bdquoOnly few old trees are standing in the

forest they look sadly down - like Noah

once did with his sons from the mountain

Ararat (Kasthofer 1822)raquo

How effective was the Bannbrief

Early deforestation and overview of

the valley (c 10th-14th century)

Bannbrief (written order) 1397 Any

use of forest product in remaining

forest is not allowed

Bildvergleich bis 2009

Geschichte des Bannwaldes

Photos Photoarchiv Xaver Buumlhlmann Andermatt

Increase of settlement and

infrastructure in the 20th

century

Increased afforestation and

forest density increasae of

forest area from 4 to 24 ha

Windthrow bdquoVivianldquo 1990

History of avalanche protection Example Andermatt

bull Increase of avalanche protection since the 19th century

bull Passive and

active afforestation

Davos ca 1940

Davos 2012

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 4: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

More irregular snow cover around trees and in forests and decrease of snow depth

Source H Imbeck (1987)

Avalanche protection ndash The role of mountain forests

Amount and duration of incoming

solar radiation are reduced in the

forest

Outgoing long-wave radiation

reduced

Avalanche protection ndash The role of mountain forests

Surface hoar is less

probable in forests

Reduction of wind speeds in the forest compared to open

areas and large gaps

Wind-transport

Source M Frehner

(from Meyer 1987 and

Cemagref)

Avalanche protection ndash The role of mountain forests

Terrain roughness of

standing and laying

stems

But critical stem densities

would be very high only with

this effect ~ 500 stems 30o

~ 1000 stems 40o (Saeki amp Matsuoka 1970 Salm 1978)

Avalanche protection ndash The role of mountain forests

Relationship between critical gap widths and crown cover densities for triggering of

avalanches for different categories of slope steepness Source Schneebeli und Bebi 2004

Crown cover ()

Avalanche protection ndash The role of mountain forests

Limits of avalache protection

Large avalanches from above the treeline can generally not be stopped by the forest

New tols for regional scale avalanche hazard mapping

Avalanche dynamic model

(RAMMS) Newly available remote sensing data

-gtImproved decicion support for management of protection forests

Evaluating protective effects against avalanches

GIS-based risk analysis R = AS P

Probability of avalanche releases Developing forest cover scenarios

bull Comparison of risks depending on forest cover scenarios

bull Determination of the value of the forest for avalanche protection (up to 150rsquo000 Euro ha and year in this case study

Mapping of forest structures

Simulating avalanche

runout

Risk calculation

R = AS P

Historic view on snow avalanche catastrophies

218 BC Hannibal crossing the Alps Loss of ca 18rsquo000 peoble by avalanches

Guides caught by avalanches at Gd St Bernard as they started while pilgrims were praying (Rudolf de St Trout 1228 )

Trento December 13th 1916 (White Friday) Ca 9000 killed people

18 Jan 2017 Rigopiano Abruzzo 19 people death

History of avalanche protection Example Andermatt

Situation in the beginning of 19th

century bdquoOnly few old trees are standing in the

forest they look sadly down - like Noah

once did with his sons from the mountain

Ararat (Kasthofer 1822)raquo

How effective was the Bannbrief

Early deforestation and overview of

the valley (c 10th-14th century)

Bannbrief (written order) 1397 Any

use of forest product in remaining

forest is not allowed

Bildvergleich bis 2009

Geschichte des Bannwaldes

Photos Photoarchiv Xaver Buumlhlmann Andermatt

Increase of settlement and

infrastructure in the 20th

century

Increased afforestation and

forest density increasae of

forest area from 4 to 24 ha

Windthrow bdquoVivianldquo 1990

History of avalanche protection Example Andermatt

bull Increase of avalanche protection since the 19th century

bull Passive and

active afforestation

Davos ca 1940

Davos 2012

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 5: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Amount and duration of incoming

solar radiation are reduced in the

forest

Outgoing long-wave radiation

reduced

Avalanche protection ndash The role of mountain forests

Surface hoar is less

probable in forests

Reduction of wind speeds in the forest compared to open

areas and large gaps

Wind-transport

Source M Frehner

(from Meyer 1987 and

Cemagref)

Avalanche protection ndash The role of mountain forests

Terrain roughness of

standing and laying

stems

But critical stem densities

would be very high only with

this effect ~ 500 stems 30o

~ 1000 stems 40o (Saeki amp Matsuoka 1970 Salm 1978)

Avalanche protection ndash The role of mountain forests

Relationship between critical gap widths and crown cover densities for triggering of

avalanches for different categories of slope steepness Source Schneebeli und Bebi 2004

Crown cover ()

Avalanche protection ndash The role of mountain forests

Limits of avalache protection

Large avalanches from above the treeline can generally not be stopped by the forest

New tols for regional scale avalanche hazard mapping

Avalanche dynamic model

(RAMMS) Newly available remote sensing data

-gtImproved decicion support for management of protection forests

Evaluating protective effects against avalanches

GIS-based risk analysis R = AS P

Probability of avalanche releases Developing forest cover scenarios

bull Comparison of risks depending on forest cover scenarios

bull Determination of the value of the forest for avalanche protection (up to 150rsquo000 Euro ha and year in this case study

Mapping of forest structures

Simulating avalanche

runout

Risk calculation

R = AS P

Historic view on snow avalanche catastrophies

218 BC Hannibal crossing the Alps Loss of ca 18rsquo000 peoble by avalanches

Guides caught by avalanches at Gd St Bernard as they started while pilgrims were praying (Rudolf de St Trout 1228 )

Trento December 13th 1916 (White Friday) Ca 9000 killed people

18 Jan 2017 Rigopiano Abruzzo 19 people death

History of avalanche protection Example Andermatt

Situation in the beginning of 19th

century bdquoOnly few old trees are standing in the

forest they look sadly down - like Noah

once did with his sons from the mountain

Ararat (Kasthofer 1822)raquo

How effective was the Bannbrief

Early deforestation and overview of

the valley (c 10th-14th century)

Bannbrief (written order) 1397 Any

use of forest product in remaining

forest is not allowed

Bildvergleich bis 2009

Geschichte des Bannwaldes

Photos Photoarchiv Xaver Buumlhlmann Andermatt

Increase of settlement and

infrastructure in the 20th

century

Increased afforestation and

forest density increasae of

forest area from 4 to 24 ha

Windthrow bdquoVivianldquo 1990

History of avalanche protection Example Andermatt

bull Increase of avalanche protection since the 19th century

bull Passive and

active afforestation

Davos ca 1940

Davos 2012

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 6: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Reduction of wind speeds in the forest compared to open

areas and large gaps

Wind-transport

Source M Frehner

(from Meyer 1987 and

Cemagref)

Avalanche protection ndash The role of mountain forests

Terrain roughness of

standing and laying

stems

But critical stem densities

would be very high only with

this effect ~ 500 stems 30o

~ 1000 stems 40o (Saeki amp Matsuoka 1970 Salm 1978)

Avalanche protection ndash The role of mountain forests

Relationship between critical gap widths and crown cover densities for triggering of

avalanches for different categories of slope steepness Source Schneebeli und Bebi 2004

Crown cover ()

Avalanche protection ndash The role of mountain forests

Limits of avalache protection

Large avalanches from above the treeline can generally not be stopped by the forest

New tols for regional scale avalanche hazard mapping

Avalanche dynamic model

(RAMMS) Newly available remote sensing data

-gtImproved decicion support for management of protection forests

Evaluating protective effects against avalanches

GIS-based risk analysis R = AS P

Probability of avalanche releases Developing forest cover scenarios

bull Comparison of risks depending on forest cover scenarios

bull Determination of the value of the forest for avalanche protection (up to 150rsquo000 Euro ha and year in this case study

Mapping of forest structures

Simulating avalanche

runout

Risk calculation

R = AS P

Historic view on snow avalanche catastrophies

218 BC Hannibal crossing the Alps Loss of ca 18rsquo000 peoble by avalanches

Guides caught by avalanches at Gd St Bernard as they started while pilgrims were praying (Rudolf de St Trout 1228 )

Trento December 13th 1916 (White Friday) Ca 9000 killed people

18 Jan 2017 Rigopiano Abruzzo 19 people death

History of avalanche protection Example Andermatt

Situation in the beginning of 19th

century bdquoOnly few old trees are standing in the

forest they look sadly down - like Noah

once did with his sons from the mountain

Ararat (Kasthofer 1822)raquo

How effective was the Bannbrief

Early deforestation and overview of

the valley (c 10th-14th century)

Bannbrief (written order) 1397 Any

use of forest product in remaining

forest is not allowed

Bildvergleich bis 2009

Geschichte des Bannwaldes

Photos Photoarchiv Xaver Buumlhlmann Andermatt

Increase of settlement and

infrastructure in the 20th

century

Increased afforestation and

forest density increasae of

forest area from 4 to 24 ha

Windthrow bdquoVivianldquo 1990

History of avalanche protection Example Andermatt

bull Increase of avalanche protection since the 19th century

bull Passive and

active afforestation

Davos ca 1940

Davos 2012

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 7: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Terrain roughness of

standing and laying

stems

But critical stem densities

would be very high only with

this effect ~ 500 stems 30o

~ 1000 stems 40o (Saeki amp Matsuoka 1970 Salm 1978)

Avalanche protection ndash The role of mountain forests

Relationship between critical gap widths and crown cover densities for triggering of

avalanches for different categories of slope steepness Source Schneebeli und Bebi 2004

Crown cover ()

Avalanche protection ndash The role of mountain forests

Limits of avalache protection

Large avalanches from above the treeline can generally not be stopped by the forest

New tols for regional scale avalanche hazard mapping

Avalanche dynamic model

(RAMMS) Newly available remote sensing data

-gtImproved decicion support for management of protection forests

Evaluating protective effects against avalanches

GIS-based risk analysis R = AS P

Probability of avalanche releases Developing forest cover scenarios

bull Comparison of risks depending on forest cover scenarios

bull Determination of the value of the forest for avalanche protection (up to 150rsquo000 Euro ha and year in this case study

Mapping of forest structures

Simulating avalanche

runout

Risk calculation

R = AS P

Historic view on snow avalanche catastrophies

218 BC Hannibal crossing the Alps Loss of ca 18rsquo000 peoble by avalanches

Guides caught by avalanches at Gd St Bernard as they started while pilgrims were praying (Rudolf de St Trout 1228 )

Trento December 13th 1916 (White Friday) Ca 9000 killed people

18 Jan 2017 Rigopiano Abruzzo 19 people death

History of avalanche protection Example Andermatt

Situation in the beginning of 19th

century bdquoOnly few old trees are standing in the

forest they look sadly down - like Noah

once did with his sons from the mountain

Ararat (Kasthofer 1822)raquo

How effective was the Bannbrief

Early deforestation and overview of

the valley (c 10th-14th century)

Bannbrief (written order) 1397 Any

use of forest product in remaining

forest is not allowed

Bildvergleich bis 2009

Geschichte des Bannwaldes

Photos Photoarchiv Xaver Buumlhlmann Andermatt

Increase of settlement and

infrastructure in the 20th

century

Increased afforestation and

forest density increasae of

forest area from 4 to 24 ha

Windthrow bdquoVivianldquo 1990

History of avalanche protection Example Andermatt

bull Increase of avalanche protection since the 19th century

bull Passive and

active afforestation

Davos ca 1940

Davos 2012

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 8: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Relationship between critical gap widths and crown cover densities for triggering of

avalanches for different categories of slope steepness Source Schneebeli und Bebi 2004

Crown cover ()

Avalanche protection ndash The role of mountain forests

Limits of avalache protection

Large avalanches from above the treeline can generally not be stopped by the forest

New tols for regional scale avalanche hazard mapping

Avalanche dynamic model

(RAMMS) Newly available remote sensing data

-gtImproved decicion support for management of protection forests

Evaluating protective effects against avalanches

GIS-based risk analysis R = AS P

Probability of avalanche releases Developing forest cover scenarios

bull Comparison of risks depending on forest cover scenarios

bull Determination of the value of the forest for avalanche protection (up to 150rsquo000 Euro ha and year in this case study

Mapping of forest structures

Simulating avalanche

runout

Risk calculation

R = AS P

Historic view on snow avalanche catastrophies

218 BC Hannibal crossing the Alps Loss of ca 18rsquo000 peoble by avalanches

Guides caught by avalanches at Gd St Bernard as they started while pilgrims were praying (Rudolf de St Trout 1228 )

Trento December 13th 1916 (White Friday) Ca 9000 killed people

18 Jan 2017 Rigopiano Abruzzo 19 people death

History of avalanche protection Example Andermatt

Situation in the beginning of 19th

century bdquoOnly few old trees are standing in the

forest they look sadly down - like Noah

once did with his sons from the mountain

Ararat (Kasthofer 1822)raquo

How effective was the Bannbrief

Early deforestation and overview of

the valley (c 10th-14th century)

Bannbrief (written order) 1397 Any

use of forest product in remaining

forest is not allowed

Bildvergleich bis 2009

Geschichte des Bannwaldes

Photos Photoarchiv Xaver Buumlhlmann Andermatt

Increase of settlement and

infrastructure in the 20th

century

Increased afforestation and

forest density increasae of

forest area from 4 to 24 ha

Windthrow bdquoVivianldquo 1990

History of avalanche protection Example Andermatt

bull Increase of avalanche protection since the 19th century

bull Passive and

active afforestation

Davos ca 1940

Davos 2012

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 9: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Limits of avalache protection

Large avalanches from above the treeline can generally not be stopped by the forest

New tols for regional scale avalanche hazard mapping

Avalanche dynamic model

(RAMMS) Newly available remote sensing data

-gtImproved decicion support for management of protection forests

Evaluating protective effects against avalanches

GIS-based risk analysis R = AS P

Probability of avalanche releases Developing forest cover scenarios

bull Comparison of risks depending on forest cover scenarios

bull Determination of the value of the forest for avalanche protection (up to 150rsquo000 Euro ha and year in this case study

Mapping of forest structures

Simulating avalanche

runout

Risk calculation

R = AS P

Historic view on snow avalanche catastrophies

218 BC Hannibal crossing the Alps Loss of ca 18rsquo000 peoble by avalanches

Guides caught by avalanches at Gd St Bernard as they started while pilgrims were praying (Rudolf de St Trout 1228 )

Trento December 13th 1916 (White Friday) Ca 9000 killed people

18 Jan 2017 Rigopiano Abruzzo 19 people death

History of avalanche protection Example Andermatt

Situation in the beginning of 19th

century bdquoOnly few old trees are standing in the

forest they look sadly down - like Noah

once did with his sons from the mountain

Ararat (Kasthofer 1822)raquo

How effective was the Bannbrief

Early deforestation and overview of

the valley (c 10th-14th century)

Bannbrief (written order) 1397 Any

use of forest product in remaining

forest is not allowed

Bildvergleich bis 2009

Geschichte des Bannwaldes

Photos Photoarchiv Xaver Buumlhlmann Andermatt

Increase of settlement and

infrastructure in the 20th

century

Increased afforestation and

forest density increasae of

forest area from 4 to 24 ha

Windthrow bdquoVivianldquo 1990

History of avalanche protection Example Andermatt

bull Increase of avalanche protection since the 19th century

bull Passive and

active afforestation

Davos ca 1940

Davos 2012

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 10: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

New tols for regional scale avalanche hazard mapping

Avalanche dynamic model

(RAMMS) Newly available remote sensing data

-gtImproved decicion support for management of protection forests

Evaluating protective effects against avalanches

GIS-based risk analysis R = AS P

Probability of avalanche releases Developing forest cover scenarios

bull Comparison of risks depending on forest cover scenarios

bull Determination of the value of the forest for avalanche protection (up to 150rsquo000 Euro ha and year in this case study

Mapping of forest structures

Simulating avalanche

runout

Risk calculation

R = AS P

Historic view on snow avalanche catastrophies

218 BC Hannibal crossing the Alps Loss of ca 18rsquo000 peoble by avalanches

Guides caught by avalanches at Gd St Bernard as they started while pilgrims were praying (Rudolf de St Trout 1228 )

Trento December 13th 1916 (White Friday) Ca 9000 killed people

18 Jan 2017 Rigopiano Abruzzo 19 people death

History of avalanche protection Example Andermatt

Situation in the beginning of 19th

century bdquoOnly few old trees are standing in the

forest they look sadly down - like Noah

once did with his sons from the mountain

Ararat (Kasthofer 1822)raquo

How effective was the Bannbrief

Early deforestation and overview of

the valley (c 10th-14th century)

Bannbrief (written order) 1397 Any

use of forest product in remaining

forest is not allowed

Bildvergleich bis 2009

Geschichte des Bannwaldes

Photos Photoarchiv Xaver Buumlhlmann Andermatt

Increase of settlement and

infrastructure in the 20th

century

Increased afforestation and

forest density increasae of

forest area from 4 to 24 ha

Windthrow bdquoVivianldquo 1990

History of avalanche protection Example Andermatt

bull Increase of avalanche protection since the 19th century

bull Passive and

active afforestation

Davos ca 1940

Davos 2012

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 11: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Evaluating protective effects against avalanches

GIS-based risk analysis R = AS P

Probability of avalanche releases Developing forest cover scenarios

bull Comparison of risks depending on forest cover scenarios

bull Determination of the value of the forest for avalanche protection (up to 150rsquo000 Euro ha and year in this case study

Mapping of forest structures

Simulating avalanche

runout

Risk calculation

R = AS P

Historic view on snow avalanche catastrophies

218 BC Hannibal crossing the Alps Loss of ca 18rsquo000 peoble by avalanches

Guides caught by avalanches at Gd St Bernard as they started while pilgrims were praying (Rudolf de St Trout 1228 )

Trento December 13th 1916 (White Friday) Ca 9000 killed people

18 Jan 2017 Rigopiano Abruzzo 19 people death

History of avalanche protection Example Andermatt

Situation in the beginning of 19th

century bdquoOnly few old trees are standing in the

forest they look sadly down - like Noah

once did with his sons from the mountain

Ararat (Kasthofer 1822)raquo

How effective was the Bannbrief

Early deforestation and overview of

the valley (c 10th-14th century)

Bannbrief (written order) 1397 Any

use of forest product in remaining

forest is not allowed

Bildvergleich bis 2009

Geschichte des Bannwaldes

Photos Photoarchiv Xaver Buumlhlmann Andermatt

Increase of settlement and

infrastructure in the 20th

century

Increased afforestation and

forest density increasae of

forest area from 4 to 24 ha

Windthrow bdquoVivianldquo 1990

History of avalanche protection Example Andermatt

bull Increase of avalanche protection since the 19th century

bull Passive and

active afforestation

Davos ca 1940

Davos 2012

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 12: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Historic view on snow avalanche catastrophies

218 BC Hannibal crossing the Alps Loss of ca 18rsquo000 peoble by avalanches

Guides caught by avalanches at Gd St Bernard as they started while pilgrims were praying (Rudolf de St Trout 1228 )

Trento December 13th 1916 (White Friday) Ca 9000 killed people

18 Jan 2017 Rigopiano Abruzzo 19 people death

History of avalanche protection Example Andermatt

Situation in the beginning of 19th

century bdquoOnly few old trees are standing in the

forest they look sadly down - like Noah

once did with his sons from the mountain

Ararat (Kasthofer 1822)raquo

How effective was the Bannbrief

Early deforestation and overview of

the valley (c 10th-14th century)

Bannbrief (written order) 1397 Any

use of forest product in remaining

forest is not allowed

Bildvergleich bis 2009

Geschichte des Bannwaldes

Photos Photoarchiv Xaver Buumlhlmann Andermatt

Increase of settlement and

infrastructure in the 20th

century

Increased afforestation and

forest density increasae of

forest area from 4 to 24 ha

Windthrow bdquoVivianldquo 1990

History of avalanche protection Example Andermatt

bull Increase of avalanche protection since the 19th century

bull Passive and

active afforestation

Davos ca 1940

Davos 2012

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 13: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

History of avalanche protection Example Andermatt

Situation in the beginning of 19th

century bdquoOnly few old trees are standing in the

forest they look sadly down - like Noah

once did with his sons from the mountain

Ararat (Kasthofer 1822)raquo

How effective was the Bannbrief

Early deforestation and overview of

the valley (c 10th-14th century)

Bannbrief (written order) 1397 Any

use of forest product in remaining

forest is not allowed

Bildvergleich bis 2009

Geschichte des Bannwaldes

Photos Photoarchiv Xaver Buumlhlmann Andermatt

Increase of settlement and

infrastructure in the 20th

century

Increased afforestation and

forest density increasae of

forest area from 4 to 24 ha

Windthrow bdquoVivianldquo 1990

History of avalanche protection Example Andermatt

bull Increase of avalanche protection since the 19th century

bull Passive and

active afforestation

Davos ca 1940

Davos 2012

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 14: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Bildvergleich bis 2009

Geschichte des Bannwaldes

Photos Photoarchiv Xaver Buumlhlmann Andermatt

Increase of settlement and

infrastructure in the 20th

century

Increased afforestation and

forest density increasae of

forest area from 4 to 24 ha

Windthrow bdquoVivianldquo 1990

History of avalanche protection Example Andermatt

bull Increase of avalanche protection since the 19th century

bull Passive and

active afforestation

Davos ca 1940

Davos 2012

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 15: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

bull Increase of avalanche protection since the 19th century

bull Passive and

active afforestation

Davos ca 1940

Davos 2012

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 16: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

ndash Increasing concerns about protection

against natural hazards during 19th

century

-gt new forest laws afforestations

ndash Decreasing values of wood in the 20th

century

ndash Development from laquoafforestationraquo to

laquoresilence maintenanceraquo

ndash Small-medium scale interventions

(mainly with cable lines)

ndash Wood production and provision of

other ecosystem services as side

product of protection forest

management

Management of avalanche protection forests in the Alps

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 17: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Other measures against avalanches

Frauenkirche Davos A protection-wedge has bin built after an avalanche destroyed the church in 1602

Stone wall (Galtuumlr Austria) build after Avalanche catastrophy in 1999

First technical measures built around 1900

Avalanche barriers made of steel (after ca 1950)

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 18: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Integral risk management against avalanches

Avalanche hazard maps

Protection forest and avalanche barriers Organisational measures

Avalanche galleries

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 19: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Windthrow

Bark beetle

Fire

Interactions with other natural disturabances

Avalanches

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 20: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Considerable effect of laying

trees

Avalanches after windthrow only very few releases

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 21: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Avalanches after windthrow long term effect

bull Decreasing avalanche protection with time bull Is development of post windthrow regeneration fast enough or

are addition afforestationstechnical measures necessary

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 22: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

How good is avalanche protection of post-fire stands

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 23: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Examples from Utah (USA)

Avalanche release on not cleared forest

fire area

Forest damage from cleared post-disturbance

area

Fotos M Jenkins Utah State University

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 24: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Interactions between

Avalanches and fire

Avalanches contribute to the diversity of the landscape and may act as fire-breaks But fine fuel after avalanches may create new fires

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 25: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Bark beetle-avalanche interactions

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 26: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

-gt Avalanches may act also as breaks for bark beetle autbreaks -gt But new release areas may occur after bark beetle disturbances

Avalanches and floods

Remaining wood in avalanche tracks along torrents may lead to floods

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 27: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Cold limited sites near

treeline

Increase of treeline and forest

density may lead to further

increase of avalanche protection

Effects of climate warming on avalanche protection forests

Other Sites

Increase of drought problems

and natural disturbances

(forest fire insects)

-gt new avalanche release

areas may occur

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 28: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

New species arrivinghelliphellip

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 29: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

The number of days with a snow

depth gt 50 cm will strongly decrease

Avalanches in forested terrrain will

generally have a decreasing

relevance compared with other

natural hazards

But Relevance of wet snow-gliding

avalanches may increase in future

Weissfluhjoch (2540 m)

Davos (1550 m)

Source Schmucki et al 2015 SLF

But is there enough snow for avalanches in forested terrain

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 30: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Avalanche-forest interactions in a warmer climate

Trends in favorable snow and weather conditions for Avalanches in forested terrain (Source Teich et al 2012)

gt1500 m asl

lt1500 m asl

Other forest avalanches

Other forest avalanches

New snow forest avalanches

New snow forest avalanches

Other forest avalanches

New snow forest avalanches

Already negative trends

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 31: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

1 Dry and cold avalanches

- After cold snowfall periods

- Mainly subalpine and more often on

N-facing slopes

Decreasing trends in

all elevations

2 Wet snow avalanches

- After warming and or rain

- Low terrain roughness

- Often in broadleaved forests often

as glide snow avalanches on S-exp

Shift of problem zones to higher

elevations

Avalanche-forest interactions in a warmer climate

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 32: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Conclusions

bull Forest management has always been an important part of integral avalanche risk management But focus is shifting towards increasing resilience and disturbance management

bull New possibilities to evaluate the value of protection forests -gt

important for priorizing the management

bull Avalanches will decrease in importance compared to other natural hazards but wet snow problems and interactions with other disturbances become more important

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4

Page 33: Avalanches: forest interactions and risk managementnetriskwork.ctfc.cat/.../uploads/2017/10/KRUMM-Frank_Forest-Avala… · avalanches for different categories of slope steepness Source:

Avalanches forest interactions and risk

management

Frank Krumm1 and Peter Bebi 12

1 WSL-Institute for Snow and Avalanche Research SLF

2 Swiss Federal Institute for Forest Snow and Landscape Research

Thank you for your attention VDLS_1_kleinmp4