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(4) Cyclonic circulation In Lake Geneva. Figure shows the observed mean current vectors recorded at around 10 m depth in the central basin of Lake Geneva.
- Source: Lemmin U and D'Adamo N (1996) Summertime winds and direct cyclonic circulation: Observations from Lake Geneva. Ann. Geophysicae, 14: 1207-1220. Reproduced with permission from European Geophysical Society
(5) Spatio-Temporal evolution of Gyres in Lake Biwa. Figures (a) and (b) shows the described gyres I, II, and III at different stages; while figure (c)from left to right and up to down shows the monthly evolution (April-Dec 1994) of the epilimniun velocities measured with ADCP transects. Gyre I was described to move south as temperature stratification became stronger and north again as the stratification weakened. Gyres II and III were not stable, varying position and size accordingly to the wind field.
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