Application of a three-dimensional numerical model to Lake
Vostok: An Antarctic subglacial lake, Geophysical Research letters

"The circulation in two water column thickness scenarios for Lake Vostok, 
a subglacial lake in central East Antarctica, is investigated using a 
three-dimensional numerical model. In a scenario with a constant water 
column thickness (the distance between the sloping ice sheet which caps 
the lake and the lake bed) the circulation is barotropic, but with a more 
realistic water column thickness the flow is baroclinic. 

The different circulations result from the geothermal heat flux warming 
shallow regions of the realistic lake more efficiently, thus forming a 
different horizontal density structure. The differences and uncertainties 
between the two scenarios highlight the importance that the largely unknown 
water column thickness and geothermal heat flux have in determining the
circulation in the lake."

http://earth.agu.org/GRL/articles/2000GL012107/GL11207W01.html


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