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Planning for Planning for Climate Climate Change Change in the in the Pacific Northwest Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington [email protected]

Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

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Page 1: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Planning for Planning for Climate ChangeClimate Change in the in the

Pacific NorthwestPacific Northwest

Amy Snover, PhDClimate Impacts Group

Center for Science in the Earth SystemUniversity of Washington

[email protected]

Page 2: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Goal: to increase the region’s resilience to climate variations and climate change

Areas of study:

Water resources Salmon Forests Coasts

The Climate Impacts The Climate Impacts GroupGroup

ColumbiaRiver Basin

- The past is the key to the future -

Page 3: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Considerations for management

Responsible management looks forward...• Needs of a growing population • Environmental stewardship • Climate change

Outline of Talk:• Brief review of climate change • Implications for Pacific Northwest climate• Consequences for PNW natural resources• Application to regional policy & planning

Page 4: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Brief Review of Climate Change

• Carbon dioxide and other greenhouse gases warm the planet

• Greenhouse gases have been increasing (CO2 up 30%) and will increase for a long time as a result of human activities

• The planet has warmed ~1°F since 1900, in part due to human activities

• Further warming of 2.5-10.4°F by 2100

Page 5: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Source: IPCC TAR 2001

Earth’s Surface Temperature - Earth’s Surface Temperature - Past and FuturePast and Future

1000 2000

+ 10°° F

+ 5°° F

1900 2100

From 1900 to 2000 the planet warmed ~1°F. Global average temperature projected to increase 2.5-10.4°F by 2100.

Very significant change from historical perspective.

Page 6: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Future Climate Change

• Earth’s average temperature projected to increase during the 21st century at a rate 2-10 times that observed in the 20th century (+2.5-10.4°F by 2100)

• Expect additional changes in climate (precipitation, storm tracks)

• Global average sea level projected to rise 4-35 inches by 2100

• These changes will have far-reaching consequences

Page 7: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Temperature Precipitation summer winter summer winter low +3.1F +3.2F -7% -2%

mean +4.7F +5.2F +2% +9% high +6.7F +6.7F +9% +22%

Warmer, wetter winters. Warmer summers.

Estimated climate change from 20th century to the 2040s using 8 climate model scenarios (“summer”=April-September, “winter” = October-March).

Climate change in the PNW

Page 8: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

PNW Temperature: Past and future

Page 9: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

The Main Impact:

Less Snow

April 1 Columbia Basin Snow Extent~ 2045Historical

Average~ 2025

Page 10: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Less snow, earlier melt: More water in winter Less water in

summerNaturalized Columbia River flow - the Dalles, OR.

winter flooding• Changes in amount &

timing of peak flows spring/summer water

temperature spring/summer flows

Changes in the Water Cycle

Columbia Basin:• Decreased spring/summer flows

-- salmon & irrigation• Increased competition & conflict

among uses • More $$ summer drought• Increased vulnerability

Page 11: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Planning for Climate Change: Municipal water

supply

0

100

200

300

400

500

600

Oct Nov Dec Jan Feb Mar Apr May Jun Jul Aug Sep

cfs

Cedar Current ClimateCedar pcm3dec4Cedar echam4dec4Cedar had2dec4Cedar had3dec4

• More winter streamflow• Less spring/summer streamflow

For western Washington rivers (Sultan, Tolt, Cedar, Green) in the 2040s:

Winter: +30 to 40%

Summer: -20 to –30%

Page 12: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Planning for Climate Change: Municipal water

supply

Demand increases with:

• population growth

• warmer temperatures

Puget Sound Region Demand Projections

50

100

150

200

250

300

350

400

450

500

550

Demand Year

Total

Pierce

Snohomish

King

Puget Sound demand changes from population projections

• More winter streamflow

• Less spring/summer streamflow

• Increased demands

Page 13: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

• More winter streamflow

• Less spring/summer streamflow

• Increased demands

Planning for Climate Change: Municipal water

supply

0

2,000

4,000

6,000

8,000

10,000

12,000

14,000

Climate impact onhydrology

Climate impact ondemand

Impact of growth ondemand 2040

Impact of climatechange on 2040

demand andhydrology

Mil

lio

n G

alll

on

s

1952196619681982198719921994

Average Monthly Bull Run Inflows1950-1999

0

200

400

600

800

1000

1200

1400

1600

1800

2000

2200

Oct Nov Dec Jan Feb Mar Apr May Jun Jul Aug Sep

Inflo

ws,

cfs

Current ClimatePCM3 2040ECHAM4 2040HadCM2 2040HadCM3 2040

2040s WATER NEEDS IN PORTLAND (OR):

Regional growth: +40 mgdClimate change: +20 mgd

Climate change impacts = 50% of growth impacts

Page 14: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Skiing Later season opening Shorter season More rainy days

4

32

1

Snoqualmie(3000’)

Stevens(4000’)

Mission Ridge(4500’)

Schweitzer(4000’)

Changes in the Water Cycle

Landslides Increased

frequency / magnitude

Exacerbated by sea level rise around Puget Sound

Page 15: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Current Conditions

Page 16: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

SalmonSalmon

• Climate influences habitat quality (stream, estuarine, and ocean habitat)

• Future scenarios indicate increased climate stress in the freshwater environment– Winter: floods– Summer/Fall: low flows & high

temperatures

• Future changes in crucial coastal and ocean habitat are uncertain

Page 17: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Big Questions:• Seasonality of precipitation change• CO2 fertilization effect

Forests

Future vegetation changes unclear• Continued forest encroachment into alpine meadows• Overall forest die-back or expansion??

Vegetation Carbon Change by 2070-2100

Page 18: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Preparing for a changing climate ...

Page 19: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

• Consider climate a component of any long-term plan

• Water: increase supply, decrease demand, increase management flexibility

• Salmon: promote biodiversity by increasing healthy and connected habitat

• Forests: maintain a full range of biodiversity

Becoming climate-wise: water, salmon, forests

Page 20: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Tools for Planning

Working with the cities of Portland & Seattle and watershed

planning leads under the 1988 Washington State Watershed

Planning Program Developing new tools for planning:

Detailed projections of potential scenarios low tech/low cost vulnerability assessments

Bringing a global issue to the local

level

Page 21: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Planning for climate change: Scenarios of future

streamflowWeb based streamflow scenario tool provides climate change

information, including free access to streamflow scenarios and data.

Partners:

Northwest Power Planning Council

Idaho Dept of Water Resources

Page 22: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

• Some global warming is very likely (1-4°F by 2040s)

• Regional warming likely to be faster than global warming (3-6°F by 2040s)

• In the PNW, climate change will:

– Reduce winter snowpack & summer streamflow

– Increase winter flooding, alter the amount and timing of streamflows with consequences for urban and irrigation water supplies, hydropower production

– Negatively affect salmon habitat, alter forest & coastal ecosystems and exacerbate some coastal hazards

• Knowledge & tools exist to support planning now.

Summary

Page 23: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Resources

Global and National Assessments (based on thousands of peer-reviewed papers):

• IPCC reports in 2001, 1996, 1990• National Academy of Sciences 2001• National Resource Council 2000• U.S. National Assessment 2001

Regional Assessments:• The Climate Impacts Group, UW

http://www.jisao.washington.edu/PNWimpacts

[email protected]

Page 24: Planning for Climate Change in the Pacific Northwest Amy Snover, PhD Climate Impacts Group Center for Science in the Earth System University of Washington

Questions?