
%0 Journal Article
%A Jacobson, G 
%A Schuett, AW 
%T Groundwater seepage and the water balance of a closed, freshwater, coastal dune lake: Lake Windermere, Jervis Bay
%J Marine and Freshwater Research
%D 1984/12/01
%V 35
%N 6
%P 645-654
%K 
%R https://doi.org/10.1071/MF9840645
%U https://www.publish.csiro.au/paper/MF9840645 
%X 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. 
