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The earlier period of Marine Isotope Stage 3 (MIS-3) prior to 48 cal ka BP was accompanied by considerable lake level drop below −95 m, whereas the lake level increase during the later period (ca. 48-29 cal ka BP) gave rise to deposition of a transgressive unit with typical of aggradational architecture in the seismic reflection profiles.
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Floating docks are helping mitigate the swings in lake level.
This short-circuiting is investigated in more detail by a 1D numerical flow and transport model of the lake calibrated with observations of lake level and lake concentrations.
Hostetler, S. W. & Bartlein, P. J. Simulation of lake evaporation with application to modeling lake level variations of Harney-Malheur Lake, Oregon.
Along with uplifting, relative lake level dropped sharply and lake accommodation was reduced, but with increased sediment supply.
During the lowstand system tract (LST), the lake level declined and the lake shrank.
The lake level is about 1.5 m below the level surrounding salt flat of Asale salt lake.
During the lacustrine expanding system tract (EST), the lake level rose quickly and the accommodation space of the lake expanded.
Early brackish lake stage: This stage represents the most humid interval, in which the lake level is high.
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