
TY  - JOUR
A1  - Jacobson, G 
A1  - Schuett, AW 
T1  - Groundwater seepage and the water balance of a closed, freshwater, coastal dune lake: Lake Windermere, Jervis Bay
JF  - Marine and Freshwater Research
JO  - Mar. Freshwater Res.
Y1  - 1984
VL  - 35
IS  - 6
SP  - 645
EP  - 654
KW  - 
UR  - https://doi.org/10.1071/MF9840645 
N2  - 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. 
ER  -

