RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 20, ES3005, doi:10.2205/2020ES000700, 2020
Figure 4. Temperature cross sections (in colour) with overlaid isohalines (contours) from the Arcona to the Gdask Basins. The result of vertical convection (up to 50 m) in the first moment of the backtracking final moment in March (left). The CIL is formed in July at starting moment of backtracking (right).
Citation: Stepanova N., A. Mizyuk (2020), Tracking the formation of the gradient part of the southeastern Baltic Sea cold intermediate layer, Russ. J. Earth Sci., 20, ES3005, doi:10.2205/2020ES000700.
Copyright 2020 by the Geophysical Center RAS.
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