RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 20, ES3005, doi:10.2205/2020ES000700, 2020

Figure 6. Temperature, salinity, and density profiles in the Gdask Basin in July 2004, 2005, 2006 near the station 22 according to the reanalysis. Red area indicates levels with tracers originating from the Bornholm Basin, green are – from the Slupsk Channel.

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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.

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