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

Figure 5. Results from backtracking in 2004 (left), 2005 (centre) and 2006 (right) (from July back to the beginning of the deep convection process) on different model levels into the CIL: initial position – green markers, resulting position – red markers.

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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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