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Change in the circulation regime in the stratified saline Lake Shira (Siberia, Republic of Khakassia)

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Abstract

The in-situ data on the vertical structure and stability of the vertical stratification of saline Lake Shira over the past decade (2007–2015) are analyzed. Simplified mathematical models have shown that strong wind in the autumn of 2014 together with rather thick ice in the winter of 2015 caused a change in the circulation regime of this water reservoir from meromictic (incomplete mixing) to holomictic (compete mixing). Based on the results obtained, a circulation regime for deep saline lakes located in the continental climate zone, in particular, in the arid zones of Southern Siberia (Khakassia, Transbaikal, and Altai) can be predicted under various climate scenarios of the future.

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Authors and Affiliations

  1. Institute of Computational Modeling, Siberian Branch, Russian Academy of Sciences, Krasnoyarsk, Russia

    V. M. Belolipetskii & S. N. Genova

  2. Institute of Biophysics, Siberian Branch, Russian Academy of Sciences, Krasnoyarsk, Russia

    A. G. Degermendzhi & D. Y. Rogozin

  3. Siberian Federal University, Krasnoyarsk, Russia

    D. Y. Rogozin

Authors
  1. V. M. Belolipetskii
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  2. A. G. Degermendzhi
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  3. S. N. Genova
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  4. D. Y. Rogozin
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Corresponding author

Correspondence to D. Y. Rogozin.

Additional information

Original Russian Text © V.M. Belolipetskii, A.G. Degermendzhi, S.N. Genova, D.Y. Rogozin, 2017, published in Doklady Akademii Nauk, 2017, Vol. 474, No. 4, pp. 486–489.

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Belolipetskii, V.M., Degermendzhi, A.G., Genova, S.N. et al. Change in the circulation regime in the stratified saline Lake Shira (Siberia, Republic of Khakassia). Dokl. Earth Sc. 474, 649–652 (2017). https://doi.org/10.1134/S1028334X17060010

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  • DOI: https://doi.org/10.1134/S1028334X17060010

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