Groundwater seepage and the water balance of a closed, freshwater, coastal dune lake: Lake Windermere, Jervis Bay
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Cyclical water-level fluctuations of up to 12 m in Lake Windermere are a response to climatic variations with a period of several years. An approximate water balance indicates that groundwater seepage is the most significant component (84%) of the outflow from the lake, whereas surface streams are the most significant component (89%) of the inflow to the lake. Groundwater flows westwards from the lake through a highly permeable Pleistocene sand aquifer.
1974 ◽
Vol 19
(1)
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pp. 73-84
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1996 ◽
Vol 26
(3)
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pp. 482-491
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2019 ◽
pp. 95-103
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