southeast alaska parks plenary #2: scientific background, drivers, and effects climate change...
TRANSCRIPT
SOUTHEAST ALASKA PARKS
PLENARY #2:SCIENTIFIC BACKGROUND,
DRIVERS, AND EFFECTS
Climate Change Planning in Alaska’s National Parks
Selecting Drivers – Key points
Drivers are the Critical forces in our scenarios planning process.
Critical forces generally have unusually high impact and unusually high uncertainty
We are aiming to create scenarios that are: Challenging Divergent Plausible Relevant
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CLIMATE SCENARIOSBIOREGION: ______________
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CLIMATE SCENARIOSBIOREGION: ______________
Avoid pairs of drivers that are too similar – think of the effects of crossing them with one another
Choose drivers that lead to the effects that are most critical
Pick drivers with a wide range of possible outcomes
Choose drivers that impact several sectors, e.g tourism, subsistence, and wildlife, not just one
Select drivers with effects in most of the parks in the network
Select drivers with a high enough likelihood to be convincing to stakeholders
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Climate Change Scenario Drivers
TEMPERATURE AND LINKED VARIABLESthaw, freeze, season length, extreme days, permafrost, ice, freshwater temperature
PRECIPITATION AND LINKED VARIABLES:rain, snow, water availability, storms and flooding,
humidity
PACIFIC DECADAL OSCILLATION (PDO)definition, effects, and predictability
SEA LEVELerosion also linked to sea ice and storms
OCEAN ACIDIFICATION
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Temperature and linked variables Temperature based on downscaled
monthly averages from SNAP Uncertainty due to GCM uncertainty,
emissions scenarios, downscaling uncertainty, PDO
Season length, freeze, and thaw dates interpolated from mean monthly temperatures
Permafrost thaw derived from ground cover, soil type, air temperature projections
Extreme days an extension of temperature trend
Sea ice and freshwater temperature also linked to air temperature
Precipitation and linked variables
Temperature based on downscaled monthly averages from SNAP Uncertainty due to GCM uncertainty,
emissions scenarios, downscaling uncertainty, PDO
Uncertainty greater than for temperature
Models do not separate rain/snow Storms include wind and precipitation
Flooding and erosion more dependent on timing than quantity
Water availability linked to precipitation and temperature
Humidity and cloud cover
Projected Winter Temperatures
2010’s
2050’s 2090’s
Projected Length of Unfrozen Season
2010’s
2050’s 2090’s
Drivers are linked to effects
Climate effects are the outcomes of the critical forces or drivers, as expressed by significant changes in particular parks. Points to consider include:
Time frame (20 years? 100 years?)Uncertainty (of both driver and effect)Severity of effect (and reversibility)Scope: what parks, who is impacted?Repercussions: what is the story?Feedback to policy
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Pacific Decadal Oscillation (PDO)
http://en.wikipedia.org/wiki/File:La_Nina_and_Pacific_Decadal_Anomalies_-_April_2008.png
Pattern of Pacific climate variability that shifts phases about every 20 to 30 years (compared to 6-18 months for ENSO)
First identified by Steven R. Hare in 1997.
Warm or cool surface waters in the Pacific Ocean, north of 20° N.
In a "warm", or "positive", phase, the west Pacific becomes cool and part of the eastern ocean warms; during a "cool" or "negative" phase, the opposite occurs.13
PDO -- Effects
Major changes in marine ecosystems correlated with PDO.
Warm eras have seen enhanced coastal ocean productivity in Alaska and inhibited productivity off the west coast of the contiguous United States.
Cold PDO eras have seen the opposite.
http://www.wrh.noaa.gov/images/fgz/science/pdo_latest.gif
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PDO -- Predictability
PDO is caused by several processes with different origins, including ENSO and more stochastic influences .
Currently NOAA has limited ability to predict PDO more than 1 year out.
Controversy exists over how PDO works, and how it might best be monitored, modeled and predicted.
Predictive strength may be improving.
http://jisao.washington.edu/pdo/
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Ocean Acidification
Reduced survival of larval marine speciesAlgae and zooplankton reducedSerious consequences for food websExact thresholds unclear
Sea Level and Storm Surges
http://seagrant.uaf.edu/map/climate/docs/sea-level.pdf
Along the southern shores of Alaska the effect so far is hardly noticeable, because most of the coastline also is slowly rising due to tectonic forces and isostatic rebound.
On the Bering Sea coast and in the Arctic, however, communities are experiencing increased damage from storm surges (extreme high water events caused by high winds and low atmospheric pressure), shoreline loss to fierce winter storms, and saltwater intrusion into freshwater sources, sanitation lagoons, and fish and wildlife habitats.
Indications are that all of this is being made worse by a gradual rise in sea level.
Survey Results
Survey asked only about the IMPORTANCE of various effects
In selecting drivers, we will also consider the UNCERTAINTY
Time frame is also an important consideration
Not all participants responded to the survey (27 responses as of this morning)
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Increasedcarbon
storage inplants
reducesatmospheric
CO2
Increased airtemperature
Averageannual
temperaturesshift from
belowfreezing to
above
Increasedprecipitation
More storms Moreavalanches
Freezing rainmore
common
Lightning andlightning-
induced fires
Air qualityimpacts fromforest fires
ATMOSPHERIC EFFECTSAv
erag
e Ra
ting
0
5
10
15
20
25
30
Increase
d carbon st
orage in
plants
reduce
s atm
ospheri
c CO2
Increase
d air t
emperature
Average
annual
temperatur
es sh
ift fro
m below fre
ezing t
o above
Increase
d precipita
tion
More sto
rms
More av
alanc
hes
Freez
ing ra
in more
common
Lightn
ing and l
ightni
ng-induce
d fires
Air quali
ty im
pacts fr
om forest
fires
3 - very important
2 - medium importance
1 - sl ightly important
0 - not important
ATMOSPHERIC EFFECTS
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Fall ing globalphytoplanktonconcentrationreduces ocean
productivityand CO2
sequestration
Freshwaterinflux from
thawingglaciersdilutes
mineral waters
Toxic marinealgae andshellfish
poisoningaffects human
and marinemammals
Oceanacidification
affectsplankton and
benthiccalcifying
fauna
Oceanacidification
reduces soundabsorption
Coastalerosion and
sea level riseincrease
frequency ofsaltwaterflooding
Stream flowsfrom melting
glaciersincrease, thendecrease over
time
Groundwatersupplies that
depend onseasonal
glacialrecharge
become lessdependable
HYDROSPHERIC EFFECTSAv
erag
e Ra
ting
0
5
10
15
20
25
30
Fallin
g global
phytoplan
kton co
ncentra
tion reduc
es oce
an prod
uctivit
y and CO2...
Fresh
water in
flux fro
m thaw
ing glacie
rs dilu
tes minera
l wate
rs
Toxic
mari
ne alga
e and sh
ellfish
poiso
ning affec
ts human a
nd m
arine m
ammals
Ocean
acidifica
tion affec
ts plan
kton an
d benthic
calcif
ying fa
una
Ocean
acidifica
tion reduc
es so
und abso
rption
Coastal
erosio
n and
sea l
evel ri
se in
crease
frequen
cy of
saltw
ater floodin
g
Strea
m flows from
melting g
lacier
s incre
ase, th
en decre
ase ove
r time
Groun
dwater su
pplies t
hat de
pend on s
easonal
glacia
l rech
arge beco
me less
d...
3 - very important
2 - sl ightly important
1 - sl ightly important
0 - not important
HYDROSPHERIC EFFECTS
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Shorter snowand iceseason
Glaciersdiminish
Glacialoutwash
affect aquaticproductivity
Glacial lakesand glacially
dammedlakes fail,
causing flashfloods
Culturalresources are
exposed assnow and ice
recede
CRYOSPHERIC EFFECTSAv
erag
e R
ating
0
5
10
15
20
25
30
Shorter snow andice season
Glaciers diminish Glacial outwashaffect aquaticproductivity
Glacial lakes andglacially dammedlakes fail , causing
flash floods
Cultural resourcesare exposed assnow and ice
recede
3 - very important
2 - medium importance
1 - sl ightly important
0 - not important
CRYOSPHERIC EFFECTS
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1.00
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Landslides and mudflows increase on steep
slopes
Earthquake activityincreases in recently
deglaciated areas
Large/small tsunamiscould result from
collapse of unstableslopes in fjords
Soil moisture declines Demand for rubble androck increases as it is
require for repairs andnew construction
LITHOSPHERIC EFFECTSAv
erag
e Ra
ting
0
5
10
15
20
25
30
Landslides andmud flows increase
on steep slopes
Earthquake activityincreases in
recentlydeglaciated areas
Large/smalltsunamis could
result fromcollapse of
unstable slopes infjords
Soil moisturedeclines
Demand for rubbleand rock increasesas it is require forrepairs and new
construction
3 - very important
2 - medium importance
1 - sl ightly important
0 - not important
LITHOSPHERIC EFFECTS
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Ecological tipping points likely to result in rapid change
Increased growing season length
Large-scale landcover changes
Vegetation expands into deglaciated coastal areas
Tree species and vegetation classes shift
Mountain and arctic ecosystems could change substantially, leading to extinctions
Drought stress affects dry forests
Atypical outbreaks of forest pests and plant diseases
Invaisve exotic speices and native species from other areas
Mature forests and 'old growth' decline
Fire increases in boreal and tundra ecosystems
BIOSPHERIC EFFECTS - vegetation and fireAv
erag
e Ra
ting
0
5
10
15
20
25
30
Ecologic
al tippin
g points
likely t
o resul
t in ra
pid chan
ge
Increase
d growing s
easo
n length
Large
-scale
landco
ver c
hang
es
Vegetati
on expan
ds into deg
laciat
ed co
astal
areas
Tree sp
ecies
and ve
getati
on clas
ses s
hift
Mountain an
d arcti
c eco
systems c
ould chan
ge su
bstan
tially, le
ading t
o extinc
t...
Drough
t stre
ss aff
ects dry
fores
ts
Atypica
l outbrea
ks of fo
rest pests
and plan
t dise
ases
Invaisv
e exoti
c speice
s and n
ative
spec
ies fr
om other are
as
Mature fo
rests
and 'o
ld growth' d
eclin
e
Fire i
ncreases
in bore
al and tu
ndra
ecosys
tems
3 - very important
2 - medium importance
1 - sl ightly important
0 - not important
BIOSPHERIC EFFECTS - vegetation and fire
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Harbor seals moveor decline
Increased ambientsound affects
marine mammals
Caribou andreindeer healthmay be affected
Fire and vegetationchanges may
increase moosehabitat
Climate changedecouples birth
timing, hinderingmoose calf
survival
Reduced snowcover reduces
survival of smallmammals
BIOSPHERIC EFFECTS - wildlife: mammalsAv
erag
e Ra
ting
0
5
10
15
20
25
Harbor sealsmove or decline
Increasedambient soundaffects marine
mammals
Caribou andreindeer healthmay be affected
Fire andvegetation
changes mayincrease moose
habitat
Climate changedecouples birth
timing,hindering
moose calfsurvival
Reduced snowcover reduces
survival ofsmall mammals
3 - very important
2 - medium importance
1 - sl ightly important
0 - not important
BIOSPHERIC EFFECTS - wildlife: mammals
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Commercial fisheries shift
Ocean acidification affects fisheries
New stream habitats become available for colonization
Fish diseases increase with rising temperatures
Some existing salmon waters may become unsuitable
Ice worm populations decline locally
Marine intertidal environments change
Exotic pests, diseases and their vectors expand
Intensified management of fisheries affects subsistence
BIOSPHERIC EFFECTS - wildlife: fish and invertebratesAv
erag
e Ra
ting
0
5
10
15
20
25
30
Commercial
fisherie
s shift
Ocean
acidifica
tion affec
ts fish
eries
New stream
habita
ts bec
ome ava
ilable
for coloniza
tion
Fish dise
ases s
uch as
Ichtyo
phonus in
crease
with ris
ing tempera
tures
Some ex
isting s
almon w
aters
may beco
me unsu
itable
Ice w
orm populati
ons dec
line lo
cally
Marine i
ntertidal
envir
onments ch
ange
Exotic p
ests,
disea
ses a
nd their
vecto
rs exp
and
Intensified
mana
gemen
t of fi
sheri
es exp
ands, a
ffecting
subsis
tence
3 - very important
2 - medium importance
1 - sl ightly important
0 - not important
BIOSPHERIC EFFECTS - wildlife: fish and invertebratesBIOSPHERIC EFFECTS - wildlife: fish and invertebrates
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Changes to terrestrial and aquatic species compositions in parks and refuges
Parks and refuges maynot be able to meet mandate of protecting current species within...
Changes in terrestrial and marine wildlife distributions affect visitor experiences
Some species suffer severe losses
Animals and plants expand into landscapes vacated by glacial ice
Predator-prey relationships change in unexpected ways
Migratory routes and destinations change
Alpine breeding birds' habitats reduced
Kittlitz's murrelet populations continue to decline
Waterfolw shifts occur as coastal ponds become more salty
Productivity of nesting shorebirds increase
Altered migration patterns make hunting more challenging
Community resources available for subsistence decline
BIOSPHERIC EFFECTS - wildlife: other issuesAv
erag
e Ra
ting
0
5
10
15
20
25
30
Change
s to te
rrestr
ial an
d aquati
c spec
ies co
mpositions in
parks an
d refuge
s
Parks a
nd refu
ges m
aynot b
e able
to m
eet man
date of p
rotecti
ng curre
nt sp...
Change
s in te
rrestr
ial an
d mari
ne wild
life dist
ributions a
ffect v
isitor
exper.
..
Some sp
ecies s
uffer sev
ere lo
sses
Animals
and plan
ts ex
pand in
to landsca
pes vaca
ted by g
lacial
ice
Predator-p
rey re
lationshi
ps chan
ge in
unexp
ected w
ays
Migrato
ry routes a
nd desti
nations
chan
ge
Alpine br
eeding
birds' h
abitats
reduce
d
Kittlitz
's murre
let populati
ons con
tinue to
declin
e
Wate
rfolw
shifts o
ccur a
s coasta
l ponds
become m
ore sal
ty
Productivit
y of n
esting s
horebirds in
crease
Altered
migrati
on patt
erns make
hunting m
ore chall
enging
Community
reso
urces a
vaila
ble for s
ubsist
ence
declin
e
3 - very important
2 - medium importance
1 - sl ightly important
0 - not important
BIOSPHERIC EFFECTS - wildlife: other issues
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Impacts to wilderness values
Tourism season lengthens
Landscape-level changes affect visitor experiences
Visitor use patterns shift
Visitor demand for new interpretive/education media products
Safety hazards develop
Predictive uses of TEK will change
Natural resource development and economic activities expand
Developmental pressures increase as snow and ice cover reduced
Infrastructre development expands along Alaska's coasts
Damage to roads, buildings, other infrastructure
Relocating indigenous communities
Aver
age
Ratin
gCOMMUNITY, TOURISM, INDUSTRY AND OTHER EFFECTS
0
5
10
15
20
25
30
Impa
cts to
wild
erness
values
Touris
m seaso
n length
ens
Landsc
ape-l
evel c
hang
es aff
ect vis
itor e
xperi
ence
s
Visitor u
se patterns s
hift
Visitor d
eman
d for n
ew in
terpre
tive/e
duca
tion media
products
Safety
hazard
s deve
lop
Predictive
uses
of TEK
will
chan
ge
Natural reso
urce dev
elopment a
nd econo
mic acti
vities e
xpan
d in Alas
ka
Developm
ental p
ressur
es incre
ase as a
n effec
t of r
educe
d snow and
ice c
over
Infrastr
uctre deve
lopment ex
pands
along Alas
ka's c
oasts
Damag
e to ro
ads, b
uildings,
other infra
struc
ture
Relocati
ng in
digeno
us com
munities
Fuel
and en
ergy pric
es incre
ase su
bstantiall
y
3 - very important
2 - medium importance
1 - sl ightly important
0 - not important
COMMUNITY, TOURISM, INDUSTRY AND OTHER EFFECTS
Critical UncertaintiesSouthwest Alaska Network (SWAN) group, August
workshop
Normal WarmerStream/lake temps
Negative
(colder)
Positive (warmer)PDO
Historical Significant increaseExtreme precip/storms
Measureable
CatastrophicOcean Acidification
Less MoreRiver basin hydrology
Less MoreWater availability
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Climate Drivers
Climate drivers are the critical forces in our scenarios planning process
Critical forces generally have unusually high impact and unusually high uncertainty
Climate drivers table specific for SE Alaska were compiled by John Walsh and Nancy Fresco of SNAP (see handouts).
All scenarios are created by examining the intersection of two drivers, creating four sectors
Selection of drivers is crucial to the planning process
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