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 Gdask 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).

      Powered by MathJax

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.

Generated from LaTeX source by ELXfinal, v.2.0 software package.