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Climate Change in the Pacific Northwest: Impacts and Planning Philip Mote UW Climate Impacts Group University of Washington Climate Science in the Public Interest
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Science of climate change Thousands of peer-reviewed scientific papers Intergovernmental Panel on Climate Change (IPCC) Major reports in 1990, 1996, 2001 Conclusions: “An increasing body of observations gives a collective picture of a warming world and other changes in the climate system.” “There is new and stronger evidence that most of the warming observed over the last 50 years is attributable to human activities.”
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Carbon dioxide: up 32%
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Methane: up 150%
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Global average temperature 18601880190019201940196019802000 0.8 0.4 0 -0.4 -0.8 degrees Celsius
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Could these measurements be wrong? Urbanization? Stations too sparse? Satellite measurements show no warming? Perhaps 10% of warming; lots of natural evidence Warming patterns very big Surface definitely warming; troposphere warming 1960- 2001 but not 1979-2001
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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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Trends in timing of spring snowmelt (1948-2000) Courtesy of Mike Dettinger, Iris Stewart, Dan Cayan +20d later –20d earlier
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Mote 2003(b) Decrease Increase
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those satellite observations Models: troposphere should warm faster than surface But satellites show little warming (0-5 miles) since 1979: does this mean that surface measurements are unreliable?
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those satellite observations Models: troposphere should warm faster than surface But satellites show little warming (0-5 miles) since 1979: does this mean that surface measurements are unreliable?
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Some evidence that it’s not natural Rate of change appears to be unusual Pattern of change matches that expected from increasing greenhouse gases Solar, volcanic forcing would have led to cooling in the past ~30 years
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Long-term context source: Mann et al., EOS
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Carbon dioxide: up 32%
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Solar output varies - but not much Figure courtesy of NOAA National Geophysical Data Center
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Natural Climate InfluenceHuman Climate Influence All Climate Influences
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Temperature change, 2071-2100 minus 1961-1990
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Main Impact: Less Snow April 1 Snow Extent for the Columbia River Basin Less snow, earlier melt: More water in winter Less water in summer
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Snake River at Ice Harbor Reduced summer flows ==> shortages for irrigation, fish, hydro; less concern over flooding Increased winter flows ==> more hydro production
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Simulated Natural Flow in the Willamette River at the Confluence with the Columbia
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Conclusions Earth is warming as greenhouse effect strengthens Regional climate change will take many forms, some of which we cannot predict Warming is virtually certain and has profound impacts: loss of snowpack, reduction in summer water supply, hardships for salmon and forests Some prudent steps can be taken now to reduce vulnerability
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Enhanced greenhouse effect
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Decrease Increase
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and climate damage Floods Estuary conditions: prey, predators, competitors Low summer streamflow, high temp ????
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Consequences Reduced summer flow in most rivers is likely More difficulty supplying water for agriculture, hydropower, fish, recreation Likelihood of snow-driven (springtime) flooding will decrease Likelihood of rain-driven (winter) flooding will increase
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21 st century temperature change IPCC (www.ipcc.ch)
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Projected PNW Climate Change 2020sTemperaturePrecipitation Low+ 0.5°C+ 1.5 % Mean+ 1.5°C+ 6.9% High+ 2.5°C+ 14.4 % 2040sTemperaturePrecipitation Low+ 1.5°C- 3.3 % Mean+ 2.3°C+ 7% High+ 3.2°C+ 13.7 % Based on an increase in equivalent CO 2 of 1% per year. Benchmarked to the decade of the 1990s. Projected changes in average annual PNW temperature and precipitation for the decades of the 2020s and 2040s.
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