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What we know about global climate change Philip Mote (206) 616-5346 philip@atmos.washington.edu philip@atmos.washington.edu University of Washington
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What we know (high confidence) Earth’s climate is changing Humans are involved and the pattern is unlike natural changes Global average temperature is likely to increase 1.4-5.8°C this century, most land areas more We know this through peer-reviewed research and assessments
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Evidence of warming Direct measurements Glaciers receding Ice shelves collapsing Snow declining and streamflow shifting Shifts in ranges and behavior of species
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Understanding recent climate history Recent trend: +0.5°C (0.9°F) in 30 yrs Human influence emerges
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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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Avoiding Dangerous Climate Change : Exeter Feb 2005 Antarctic Peninsula Glacier Acceleration “cork from bottle” analogy Larsen A – x3 increase in flow speed of 2 feed glaciers Larsen B – x2-x6 increase in flow speed of 4 feed glaciers Hektoria glacier lowered by ~40m in 6 mo Glaciers south of collapse region unaffected ~ 0.06mm/y global msl contribution? Work in progress
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Rapid global sea level rise
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11 Local evidence of warming
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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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3.6°F 2.7°F 1.8°F 0.9°F
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Puget Sound area
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Race Rocks lighthouse, Victoria
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As the West warms, winter flows rise and summer flows drop Figure by Iris Stewart, Scripps Inst. of Oceanog. (UC San Diego)
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Stewart et al., 2004; Stewart et al., 2005 Spring-pulse dates Centers of Mass By several measures, Western snowfed streamflow has been arriving earlier in the year in recent decades Spring pulse Center time
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April 1 snowpack: no decline at high elevations
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...but large declines at low elevations
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Green daily flow records dating to <1935
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Metrics of flow Center date JJAS flow
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Center date of annual flow As observed elsewhere, mean inflow to Puget Sound is shifting earlier as the snowpack declines
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Data from Climate Monitoring and Diagnostics Lab., NOAA. Data prior to 1973 from C. Keeling, Scripps Inst. Oceanogr. Changing atmospheric composition: CO 2 Mauna Loa, Hawaii
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Carbon dioxide: up 32%
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Natural Climate InfluenceHuman Climate Influence All Climate Influences
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Climate change commitment: at any point in time, we are committed to additional warming and sea level rise from the radiative forcing already in the system: the brakes work slowly! (Meehl et al., 2005: How much more warming and sea level rise? Science, 307, 1769—1772)
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Recent findings and events zOcean acidification zIntensity and destructiveness of tropical cyclones may be increasing (controversial) zUnprecedented 2003 European heat wave may have been accentuated by warming
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Hurricane Catarina - first recorded South Atlantic tropical storm, March 2004
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Total: 27 (vs 21 in 1933) Total: 13 (vs 12 in 1969)
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Conclusions zHuman influence on climate has emerged zWarming and its consequences will continue even after greenhouse gas concentrations are stabilized z
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