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

Figure 1. The Cold Intermediate Layer in the Baltic Proper. (a) Schematic profiles of temperature, salinity, density and temperature of maximum density in the southeastern part of the Baltic Sea. The horizontal black lines mark upper and lower boundaries of the CIL. A dashed line separates the quasi-homogeneous salinity sublayer from the gradient salinity sublayer of the CIL. (b) A schematic vertical cross-section in the temperature field on the main section of the Baltic Sea in summer (based on Monitoring Cruise of Baltic Sea Research Institute Warnemünde [http://www.io-warnemuende.de]). A black rectangle marks the area of the CIL.

 
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.