ISSN 2070-7401 (Print), ISSN 2411-0280 (Online)
Sovremennye problemy distantsionnogo zondirovaniya Zemli iz kosmosa
CURRENT PROBLEMS IN REMOTE SENSING OF THE EARTH FROM SPACE

  

Sovremennye problemy distantsionnogo zondirovaniya Zemli iz kosmosa, 2026. Т. 23. № 3. С. 328-341

Elements of mesoscale water dynamics in the eastern part of the Middle Caspian: satellite observations, in situ measurements, modeling results

A.I. Ginzburg 1 , A.G. Kostianoy 1, 2, 3 , N.A. Sheremet 1 
1 Shirshov Institute of Oceanology RAS, Moscow, Russia
2 Moscow Witte University, Moscow, Russia
3 Maykop State Technological University, Maykop, Russia
Accepted: 28.04.2026
DOI: 10.21046/2070-7401-2026-23-3-328-341
The paper compares certain elements of mesoscale circulation of surface waters in the eastern Middle Caspian (warm jet streams from the South to the Middle Caspian and currents in the coastal upwelling zone) identified through the analysis of satellite images of sea surface temperature (SST) from different years, with known results of in situ measurements and numerical modeling using eddy-resolving hydrodynamic models. Good agreement is noted between the spatiotemporal characteristics of two types of jets in the South Caspian (propagating along the periphery of the cyclonic gyre over the Derbent Depression in October–June and along the eastern coast within approximately the 50-meter isobath in July–September) identified during satellite monitoring, and the results of numerical modeling. Using daily SST maps from the GHRSST (Group for High Resolution Sea Surface Temperature) project, the movement of the South Caspian water jet was traced in August 2014 to approximately the latitude of Cape Peschaniy and then, in the form of a thinner jet with lower SST, to the southern coast of the Tyub-Karagan Peninsula. The estimated propagation velocity of the South Caspian jet based on SST maps (approximately 12–22 cm/s at different stages of its northward progress) also agrees well with the model-estimated average monthly velocity (approximately 8–12 cm/s). The unusual northward propagation of the transverse upwelling jet observed in successive satellite images in September 2003 can be explained by taking into account known instrumental measurements of the current structure during winds unfavorable for upwelling.
Keywords: Caspian Sea, Middle Caspian Sea, South Caspian Sea, seasonal coast upwelling, water advection, jet streams, sea surface temperature, satellite observations, numerical modeling, eddy-resolving hydrodynamic models
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