Summer thermal structure and anticyclonic circulation of Lake Erie

被引:46
作者
Beletsky, Dmitry [1 ]
Hawley, Nathan [2 ]
Rao, Yerubandi R. [3 ]
Vanderploeg, Henry A. [2 ]
Beletsky, Raisa [1 ]
Schwab, David J. [2 ]
Ruberg, Steven A. [2 ]
机构
[1] Univ Michigan, Sch Nat Resources & Environm, CILER, Ann Arbor, MI 48108 USA
[2] NOAA, Great Lakes Environm Res Lab, Ann Arbor, MI 48108 USA
[3] Environm Canada, Natl Water Res Inst, Burlington, ON L7R 4A6, Canada
关键词
GREAT-LAKES; MEAN CIRCULATION; ROTATING FLUID; CENTRAL BASIN; WIND; CURRENTS; MOTIONS; STRATIFICATION; GENERATION; TOPOGRAPHY;
D O I
10.1029/2012GL051002
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
In most thermally stratified lakes, the summer thermocline has the shape of a "dome", with a shallower depth offshore than nearshore. This configuration is accompanied by a lake-wide cyclonic circulation. Lake-wide observations of subsurface temperature in central Lake Erie revealed an atypical "depressed" or "bowl-shaped" thermocline in late summer, with a deeper thermocline in the middle of the lake and a shallower thermocline nearshore. Currents measured in the central basin when the bowl-shaped thermocline was observed were anticyclonic, forming a single basin-wide gyre. It is suggested that the unusual bowl-shaped thermocline is the result of Ekman pumping driven by anticyclonic vorticity in surface winds. The bowl-shaped thermocline can lead to greater hypoxia in bottom waters and negative effects on biota by reducing the hypolimnetic volume. Citation: Beletsky, D., N. Hawley, Y. R. Rao, H. A. Vanderploeg, R. Beletsky, D. J. Schwab, and S. A. Ruberg (2012), Summer thermal structure and anticyclonic circulation of Lake Erie, Geophys. Res. Lett., 39, L06605, doi:10.1029/2012GL051002.
引用
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页数:6
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