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The Arctic Climate Paquita Zuidema, RSMAS/MPO, MSC 118, March 2 2007
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29 Aug 1980
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First some pure observations…
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Change in annual mean temperature (°C): 1956-2005
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Global temperature anomalies in 2005 relative to 1951-1980
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Changes of Alaskan station temperatures (F), 1949-2004 [ from Alaska Climate Research Center ]
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[from G. Juday, UAF]
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Record Arctic sea ice minima: 2002- 2005
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29 Aug 1980
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25 Aug 2005
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6 Sep 2006
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Submarine- measured sea ice thickness
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Age of sea ice in the Arctic Ocean: 1988- 2005
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Cumulative volume changes of glaciers (ACIA, 2005) North America Scandinavia Russia No. Hemis.
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Extent of summer melt on Greenland
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Satellite data tells us sea-level heights, since 1992 a rise of about 2 cm
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annual Increased Spring And Summer Cloudiness 1982-1999 AVHRR data (Wang&Key, 2003) Persistent springtime cloud cover may advance snowmelt onset date (e.g., modeling study of Zhang 1996) spring summer
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Now some future model projections…
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Permafrost (CCSM) Sept. sea-ice (CCSM) Sept. sea-ice (Observed) (Holland, Lawrence)
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Projected changes of temperature: 2070- 2090
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Projected changes of Arctic sea ice
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IPCC models: Arctic sea ice coverage, 1950- 2100
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IPCC models: Projected Arctic (60-90ºN) change of surface air temperature relative to 1980-2000
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Impact of 1 meter (3 feet) sea level rise on FL
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What are we doing about it (as scientists) ?
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8 years of data from the North Slope of Alaska DOE/ARM site
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SHEBA Surface Heat Budget of the Arctic
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Early May ~ 76N, 165 W
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annual Increased Spring And Summer Cloudiness 1982-1999 AVHRR data (Wang&Key, 2003) Persistent springtime cloud cover may advance snowmelt onset date (e.g., modeling study of Zhang 1996) spring summer
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Surface-based Instrumentation: May 1-8 time series dBZ 35 GHz cloud radar ice cloud properties depolarization lidar-determined liquid cloud base Microwave radiometer-derived liquid water paths 4X daily soundings. Near-surface T ~ -20 C, inversion T ~-10 C -5-45 -20 1 2345678 day z -30C 4 1 8 2 4 6 8 km 100 g/m^2 day -10C lidar cloud base
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May 4 Cloud Particle Imager data …pristine ice particles from upper cloud...super-cooled drizzle
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How do clouds impact the surface ? J noon = 60 o Clouds decrease surface SW by 55 W m -2,increase LW by 49 W m -2 Surface albedo=0.86; most SW reflected back Clouds warm the surface, relative to clear skies with same T& T & RH, by time-mean 41 W m -2* (little impact at TOA) Can warm 1m of ice by 1.8 K/day, or melt 1 cm of 0C ice per day, barring any other mechanisms !
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Great websites with real-time data, historical fotos: http://www.arctic.noaa.gov/ http://nsidc.org http://nsidc.org/cryosphere/glance http://nsidc.org/data/seaice-index/
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Thank you ! Paquita Zuidema, RSMAS/MPO, MSC118, March 2 2007
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