Abstract
The INMIO-CICE hydrodynamic model of the Caspian Sea was used to calculate equilibrium river runoff and evaporation from the sea surface over a wide range of sea levels (from –85 to +50 m a.s.l.) for different climatic conditions: the Last Glacial Maximum (about 21 ka BP) and the pre-industrial climate (~1850). Data from the INMCM4.8 climate model were used as boundary conditions. It was found out that a river runoff of about 400 km3/yr was required in the Last Glacial Maximum to maintain the sea level at 35–50 m a.s.l. corresponding to the maximum values of the Khvalynian transgression. In the Last Glacial Maximum, evaporation from the sea surface decreased by 105–175 mm (12–22%), and a precipitation layer, according to the INMCM4.8 model, decreased by 50–70 mm (15–30%). These conditions caused the equilibrium runoff to decrease by about 10–20% compared to the pre-industrial conditions. Smaller absolute and relative changes corresponded to lower sea levels. The maximum evaporation decrease occurred at 5 m a.s.l.
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Funding
The work was supported by the Russian Science Foundation (grant no. 19-17-00215, modeling of CS WB components; grant no. 23-62-10043, INMCM4.8 simulations and data processesing) and the State Assignment (project no. FMWS-2024-0001, analysis of CS WB components and climate data).
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Translated by E. Maslennikova
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Morozova, P.A., Ushakov, K.V., Semenov, V.A. et al. Water Balance of the Caspian Sea in the Last Glacial Maximum and Pre-Industrial Conditions Based on the Experiments with the INMIO-CICE General Sea Circulation Model. Dokl. Earth Sc. 515, 675–679 (2024). https://doi.org/10.1134/S1028334X23603620
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DOI: https://doi.org/10.1134/S1028334X23603620