RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 20, ES3005, doi:10.2205/2020ES000700, 2020
Figure 6. Temperature, salinity, and density profiles in the Gdask 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.
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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