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Rapid Warming of Lake Superior and the role of ice. Jay Austin and Steve Colman Depts. of Physics & Geol. Sci. and Large Lakes Observatory University of Minnesota Duluth MSU ESP Workshop 9 April, 2008. 45006. * 45001. * 45004. * 45006. NOAA’s NDBC buoys. Three buoys in Lake Superior
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Rapid Warming of Lake Superior andthe role of ice Jay Austin and Steve Colman Depts. of Physics & Geol. Sci. and Large Lakes Observatory University of Minnesota Duluth MSU ESP Workshop 9 April, 2008
45006 * 45001 * 45004 * 45006
NOAA’s NDBC buoys • Three buoys in Lake Superior • 1979-Present • April-November • AT,WT, WS/WD • Frequently calibrated • (also buoys in other lakes)
NDBC 45001 (Central) Water Temperature (Max. Temperatures) ~0.12C/yr
Regional Air Temperature 15 14 Regional Air Temp, C ~0.06C/yr 13 12 1980 1985 1990 1995 2000 2005
Summer Water Temperature depends on last winter’s ice cover (1998)
Amplification of summer warming • Warmer, windier(?) winters • Less ice cover • Ice-albedo feedback, less ice • Earlier summer turnover • Longer stratified (heating) season • Warmer summer air temps, acting over a longer heating season = amplification
Is the effect strong enough? ~0.11C/yr ~1 ~0.06C/yr ~ -0.015C/% ~ -0.42%/yr ~0.06C/yr ~0.063C/yr
Comparing SSM to globe ~0.1C/yr
Fitting it together? • Increased WT • Due to warmer summers, reduced ice cover • Increased Wind Speeds • Due to warmer water Temperatures (?) • Decreased ice cover • Due to milder winters, higher winds (?) • Decreased lake levels • Due to higher WT, higher winds, reduced ice cover • Highly sensitive, non-linear system