Characterization of the bottom turbid layer in a pit lake and its response to convective cooling
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American Society of Limnology and Oceanography2002
[1] During the winters of 1998 and 1999, observations were made of the cascading of cold water from the nearshore, shallow "shelf'' zones and down the sloping sides of Lake Geneva. Cascading starts on the average 10 hours after the onset of surface cooling ...
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