Lake Superior summer water temperatures are increasing more rapidly than regional air temperatures: A positive ice-albedo feedback

被引:392
|
作者
Austin, Jay A.
Colman, Steven M.
机构
[1] Univ Minnesota, Large Lakes Observ, Duluth, MN 55812 USA
[2] Univ Minnesota, Dept Phys, Duluth, MN 55812 USA
[3] Univ Minnesota, Dept Geol Sci, Duluth, MN 55812 USA
关键词
D O I
10.1029/2006GL029021
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Lake Superior summer ( July - September) surface water temperatures have increased approximately 2.5 degrees C over the interval 1979 - 2006, equivalent to a rate of ( 11 +/- 6) x 10(-2) degrees C yr(-1), significantly in excess of regional atmospheric warming. This discrepancy is caused by declining winter ice cover, which is causing the onset of the positively stratified season to occur earlier at a rate of roughly a half day per year. An earlier start of the stratified season significantly increases the period over which the lake warms during the summer months, leading to a stronger trend in mean summer temperatures than would be expected from changes in summer air temperature alone.
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