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Global Warming and Its impacts on the Pacific Northwest Dr. Nathan Mantua University of Washington Climate Impacts Group Dr. Nathan Mantua University of Washington Climate Impacts Group For the NW Straits Commission The Skagit Casino and Resort November 4, 2005
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cses.washington.edu/cigcses.washington.edu/cig Columbia River Basin The Climate Impacts Group A NOAA-funded research and education team at the University of Washington
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The Greenhouse Effect There is a natural greenhouse effect that warms the earth’s average surface temperature by ~33 C Pierce
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The natural Greenhouse Effect
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Humans are increasing the greenhouse effect by adding greenhouse gases to the atmosphere CO 2 : by 32% Methane: by 150% Nitrous oxide: by 17% IPCC 2001
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From Jones and Palutikof http://www.cru.uea.ac.uk/cru/info/warming/ Global Average Surface Temperatures are Rising ~0.8 C rise in global average temperatures since 1860s
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3.6°F 2.7°F 1.8°F 0.9°F cooler warmer Temperature trends (°F per century) since 1920
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Evidence of warming Ice is melting everywhere
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Larsen B Ice shelf Antarctica January 31, 2002 MODIS data Courtesy NSIDC
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February 17
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February 23
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March 5
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1928 2000 The South Cascade glacier retreated dramatically in the 20th century Courtesy of the USGS glacier group
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Declining April 1 snowpack, 1950-1997
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1950-1997 relative trends in April 1 SWE vs DJF temperature Obs VIC
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Stewart et al., 2005 Spring-pulse dates Centers of Mass Western snowfed streamflow has been arriving earlier in the year in recent decades Spring pulse Center time Figure by Iris Stewart, Scripps Inst. of Oceanog. (UC San Diego)
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Natural Climate InfluenceHuman Climate Influence All Climate Influences
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What about the future?
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22 Pop-culture perspectives Perhaps this is good fiction, but it is not good science Likewise, the Day After Tomorrow scenario might make for a fun movie, but it presents physically impossible impacts of global warming at ridiculous rates of change
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21 st century Global Average temperature change Scenarios IPCC (www.ipcc.ch) social unknowns and emissions geophysics uncertainty
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Temperature change, 2071-2100 minus 1961-1990
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21 st Century PNW Temperature Change Scenarios
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Springtime snowpack will decline, especially at the warmest locations +2.3C, +4.5% winter precip + 4.1 ºF (2.3 º C) & + 4.5% winter precipitation
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The coldest locations are less sensitive to warming + 4.1°F + 4.5% winter precip
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Runoff patterns are temperature and Elevation dependent Oct Feb Jun Skagit Puyallup Skokomish Oct Feb Jun Puget Sound Precip Oct Feb Jun 1900’s a warmer climate
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Sea Level Rise scenarios depend on regional tectonics tectonic processes and glacial rebound are causing South Puget Sound to subside and the Olympic Peninsula to uplift this means that relative sea level rise will be greatest in South Puget Sound (~3.3ft by 2100), and least near Neah Bay (~1.3ft by 2100)
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Climate impacts on salmon must be added to existing stresses across their full life-cycle
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HABITAT CHANGE and DEGRADATION INCLUDING GLOBAL WARMING HATCHERY PRACTICES HARVEST PRACTICES Impacts are cumulative …
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Temperature thresholds for coldwater fish in freshwater Warming temperatures will increasingly stress coldwater fish in the warmest parts of our region A monthly average temperature of 68ºF (20ºC) has been used as an upper limit for resident cold water fish habitat, and is known to stress Pacific salmon during periods of freshwater migration, spawning, and rearing. +3.4 °F +4.1 °F
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Climate change impacts on Washington’s forests CO 2 fertilization A transient impact a longer dry season reduced regeneration, increased vulnerability to fires and pests (except in especially cool-wet locations) shifts in species ranges subalpine forests “invading” alpine meadows; a northward march--or a loss--of species?
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Ecosystem thresholds: the case of the Mountain Pine Beetle a massive outbreak of the mountain pine beetle in BC has killed 100 billion board feet (approx. 9 years of harvest) low temperatures (< -10°F) limit beetle activity a recent lack of extreme cold, killing temperatures has allowed the beetle to thrive in epidemic numbers beetle killed pines in BC Photos from http://www.for.gov.bc.cal
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Climate change sharpens the tradeoffs in a world of multiple stresses climate change will likely intensify existing conflicts over scarce natural resources o most of our natural resources are now fully allocated and managers already grapple with difficult tradeoffs o summer water supplies for in and out of stream uses are especially vulnerable to climate warming global warming impacts on the PNW depend on both the climate change and on how we prepare
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Choices now Reduce emissions - makes a big difference beyond 2050 Prepare for impacts - anticipating change may enhance benefits, minimize risks, and make it more likely to reach planning goals o Examples: city water supplies, salmon recovery plans, habitat conservation and restoration plans, coastal development …
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Main points Global climate is changing under human influence Some effects are already being observed Future effects a mix of bad and good, and will in part depend on policy decisions now
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