new techniques for quantifying patch dynamics in rivers to ... · rivers to support baseline...

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“… “… habitat evolves through natural and anthropogenic processes, and habitat evolves through natural and anthropogenic processes, and patterns of change may be as important as any other habitat attr patterns of change may be as important as any other habitat attr ibute ibute - - Naiman and Latterell 2005 Naiman and Latterell 2005 Josh Latterell Josh Latterell New techniques New techniques For quantifying patch dynamics in For quantifying patch dynamics in rivers to support baseline monitoring rivers to support baseline monitoring

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Page 1: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects

“…“…habitat evolves through natural and anthropogenic processes, andhabitat evolves through natural and anthropogenic processes, andpatterns of change may be as important as any other habitat attrpatterns of change may be as important as any other habitat attributeibute””

--Naiman and Latterell 2005Naiman and Latterell 2005

Josh LatterellJosh Latterell

New techniques New techniques For quantifying patch dynamics in For quantifying patch dynamics in rivers to support baseline monitoringrivers to support baseline monitoring

Page 2: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects

BaselineBaseline monitoringmonitoring

Goal Goal –– Characterize existing ecological conditions for Characterize existing ecological conditions for

future comparisons (effectiveness monitoring)future comparisons (effectiveness monitoring)

Two time periods Two time periods –– PrePre--impactimpact–– Post impactPost impact–– (Restored)(Restored)

ScaleScale–– Segment (20Segment (20--30 x channel width)30 x channel width)

Page 3: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects

Study siteStudy site

Page 4: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects

Study siteStudy site

Page 5: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects

PatchPatch turnoverturnover

Dynamic patch mosaicDynamic patch mosaic

Transfers important Transfers important materialsmaterials

Driven by channel Driven by channel migration, successionmigration, succession

Page 6: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects
Page 7: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects
Page 8: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects
Page 9: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects
Page 10: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects
Page 11: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects
Page 12: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects
Page 13: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects
Page 14: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects
Page 15: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects

MethodsMethods

AirphotosAirphotos–– 4 pre4 pre--impactimpact–– 4 post4 post--impactimpact

Channel migration:Channel migration:–– Sequential centerline differencing (SCD)Sequential centerline differencing (SCD)

Patch dynamics:Patch dynamics:–– Cumulative erosion rate (CER)Cumulative erosion rate (CER)

Page 16: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects

SCD Technique:SCD Technique: 1. Establish belt transects (300 ft)1. Establish belt transects (300 ft)

Page 17: New Techniques for Quantifying Patch Dynamics in Rivers to ... · rivers to support baseline monitoring. ... – Cumulative erosion rate (CER) SCD Technique: 1. Establish belt transects

2. Delineate and subdivide initial channel centerline2. Delineate and subdivide initial channel centerline

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3. Delineate and subdivide next channel centerline3. Delineate and subdivide next channel centerline

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4. Quantify distance, mechanism, and direction of change4. Quantify distance, mechanism, and direction of change

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5. Calculate average in each belt transect5. Calculate average in each belt transect

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6. Repeat for sequential channel positions, average over all int6. Repeat for sequential channel positions, average over all intervalservals

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Results Results -- PrePre--impactimpact

Pre-impact (1936-1970*)

-100 -50 0 50 100

6000

5400

4800

4200

3600

3000

2400

1800

1200

600

Valle

y po

sitio

n (ft

)

Rate of channel movement (ft/yr)

Meandering (R)Meandering (L)Switching (R)Switching (L)Indeterminate (R)Indeterminate (L)Avulsion (R)Avulsion (L)

River left River right

Mechanisms

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Post-impact (1970-2007)

-100 -50 0 50 100

6000

5400

4800

4200

3600

3000

2400

1800

1200

600

Valle

y po

sitio

n (ft

)

Rate of channel movement (ft/yr)

Meandering (R)Meandering (L)Switching (R)Switching (L)Indeterminate (R)Indeterminate (L)Avulsion (R)Avulsion (L)

Levees, railroad prism Contact with valley wall

River left River right

Mechanisms

Results Results -- Post ImpactPost Impact

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Patch Erosion Rates:Patch Erosion Rates: 1. Classify 1. Classify initialinitial landcoverlandcover

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2. Establish PRE2. Establish PRE--IMPACT sampling pointsIMPACT sampling points

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3. Track fate of each sampling point3. Track fate of each sampling point

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4. Classify POST4. Classify POST--IMPACT IMPACT landcoverlandcover, new sampling pts, new sampling pts

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5. Track fate of each sampling point5. Track fate of each sampling point

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ResultsResults

Pioneer bar

0%

50%

100%

0 10 20 30 40 50 60 70

Time (t)

Per

cent

rem

aini

ng Pre-ImpactPost-ImpactPre-impactReferencePost-impact

y = e-0.0059(t)

r 2 = 0.89

y = e-0.0316x

r 2 = 0.97

•• 81%81% decline in turnover ratedecline in turnover rate•• Used to last 22 yrs, now last 117 yearsUsed to last 22 yrs, now last 117 years•• Indicative of Indicative of terrestrializationterrestrialization

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ResultsResults

Terrace

0%

50%

100%

0 10 20 30 40 50 60 70

Time (t)

Per

cent

rem

aini

ng Pre-ImpactPost-ImpactPre-impactReferencePost-impact

y = e-0.0057(t)

r 2 = 0.78

y = e-0.0123x

r 2 = 0.97

•• 54%54% decline in turnover ratedecline in turnover rate•• Used to last 56 yrs, now last 122 yearsUsed to last 56 yrs, now last 122 years

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Patch turnover delivers large woodPatch turnover delivers large wood

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Replenishes spawning gravelsReplenishes spawning gravels

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Maintains young forestsMaintains young forests

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Nutritious leaf litterNutritious leaf litter

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ConclusionsConclusionsReduced meandering by 4 ft/yr (from 0Reduced meandering by 4 ft/yr (from 0--3900 ft), especially river left3900 ft), especially river left

-30

-25

-20

-15

-10

-5

0

5

10

15

6000

5700

5400

5100

4800

4500

4200

3900

3600

3300

3000

2700

2400

2100

1800

1500

1200900

600

300

Valley position (ft)

Cha

nge

in p

roce

ss ra

te (f

t/yr)

Meandering (R)Meandering (L)

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ConclusionsConclusionsReduced switching by 11Reduced switching by 11--14 ft/yr (from 270014 ft/yr (from 2700--6000 ft)6000 ft)

-80

-70

-60

-50

-40

-30

-20

-10

0

10

20

6000

5700

5400

5100

4800

4500

4200

3900

3600

3300

3000

2700

2400

2100

1800

1500

120090

0

600

300

Valley position (ft)

Cha

nge

in p

roce

ss ra

te (f

t/yr)

Switching (R)Switching (L)

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ConclusionsConclusionsPatches erode more slowly, last longerPatches erode more slowly, last longerYoung forests in declineYoung forests in decline

--62%62%--54%54%TerraceTerrace0%0%--45%45%FloodplainFloodplain

--92%92%--81%81%Pioneer barPioneer bar

Change in Change in eroded areaeroded area

Change in Change in erosion rateerosion rate

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Ecological consequencesEcological consequences

WoodWood•• --250 m250 m3 3 yy--1 1

•• --15,000 pieces (mostly small)15,000 pieces (mostly small)

SedimentSediment•• --11,000 CY y11,000 CY y--11 (rough estimate)(rough estimate)

Soil NSoil N•• --200 kg N y200 kg N y--1 1

•• Amount in roughly 1,000 salmon carcassesAmount in roughly 1,000 salmon carcasses

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Next stepsNext steps

Field surveys to quantify ecological Field surveys to quantify ecological consequencesconsequencesEffectiveness monitoringEffectiveness monitoring–– PostPost--restorationrestoration–– Structural changesStructural changes–– Changes in process ratesChanges in process rates

Will we see a return to preWill we see a return to pre--impact conditions?impact conditions?

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Supported by a grant fromSupported by a grant from