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• W2025145846 endingPage "514" @default.
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• W2025145846 abstract "Currents and water temperatures were recorded at a large-scale grid of fixed moorings in Lake Erie from May 1979 through June 1980. Currents measured in the lower half of the central basin water column were mostly return flows (beneath the surface wind drift) driven by the surface pressure gradient. Often observed was a complex system of Lake Erie circulation gyres as predicted by models. Another common occurrence was for one of the central basin gyres to become dominant and envelop the whole basin in either uniform clockwise or anticlockwise flow. It is not fully certain why one of the circulation cells grows as opposed to the others, but the curl of the wind stress had influence. The currents were more barotropic than predicted by full Ekman layer current models. Tidal-like currents driven by the longitudinal seiches of Lake Erie dominate the island-filled passages between the western and central Lake Erie basins, with currents across the whole island chain very closely in phase. Processes of hypolimnion volume entrainment are suggested from the central basin temperature recordings. Large volume water exchanges between the central and eastern basins occurred after the water mass in the vicinity of the shallow ridge that separates them had become unstratified. These and other topics are discussed as the large data set generated from the experiment is explored." @default.
• W2025145846 created "2016-06-24" @default.
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• W2025145846 date "1987-01-01" @default.
• W2025145846 modified "2023-10-10" @default.
• W2025145846 title "Studies of Large-Scale Currents in Lake Erie, 1979–80" @default.
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• W2025145846 doi "https://doi.org/10.1016/s0380-1330(87)71668-2" @default.
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