MODELING OF WATER CIRCULATION IN THE ANTARCTIC SUBGLACIAL LAKE VOSTOK


https://doi.org/10.15356/2076-6734-2012-4-86-91


Abstract

Different ways of defining the characteristics of Antarctic subglacialLakeVostokcirculation are considered. The disadvantages of hydrodynamic models using the hydrostatic approximation exposed to analysis. Differential equations and boundary conditions of three-dimensional nonhydrostatic model in terms vorticity–vector potential, specially developed for the modelling of the lake circulation are presented. 3D model passed through the testing by means simulations of convective currents in the simple-form reservoirs. On the basis of the seismic data on the thickness of a glacier and bathimetry of the lake the computational domain approximating a water body ofLakeVostokis constructed. Some results of modeling of the convective processes in the lake, obtained at the initial stage of circulation evolution using finite-difference grid with a spatial resolution of 8000 × 1500 ×30 mare shown.


About the Authors

G. V. Kazko
Arctic and Antarctic Research Institute, Sankt-Petersburg
Russian Federation


L. M. Savatyugin
Arctic and Antarctic Research Institute, Sankt-Petersburg
Russian Federation


I. N. Sokratova
Arctic and Antarctic Research Institute, Sankt-Petersburg
Russian Federation


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Supplementary files

For citation: Kazko G.V., Savatyugin L.M., Sokratova I.N. MODELING OF WATER CIRCULATION IN THE ANTARCTIC SUBGLACIAL LAKE VOSTOK. Ice and Snow. 2012;52(4):86-91. https://doi.org/10.15356/2076-6734-2012-4-86-91

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ISSN 2076-6734 (Print)
ISSN 2412-3765 (Online)