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

Physics

Scientific paper

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Cryosphere: Lakes (9345), Global Change: Impacts Of Global Change (1225), Global Change: Regional Climate Change, Hydrology: Limnology (0458, 4239, 4942), Oceanography: General: Limnology (0458, 1845, 4942)

Scientific paper

Lake Superior summer (July-September) surface water temperatures have increased approximately 2.5°C over the interval 1979-2006, equivalent to a rate of (11 +/- 6) × 10-2°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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