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

Article Map

• Abstract
• 1. Introduction
• 2. Materials and Methods
• 3. Results and Discussion
  • 3.1. How Well is the CIL Reproduced by the Model: Comparison With the Field Data?
  • 3.2. Formation the Salinity Gradient Sublayer of the CIL Based on Backtracking Results
• 4. Conclusions
• Acknowledgment

• Figure 1. The Cold Intermediate Layer in the Baltic Proper. (a) Schematic...
• Figure 2. Left – Baltic Proper bathymetry in colour. A white...
• Figure 3. (a) Location of the CIL boundaries and the maximum of salinity...
• Figure 4. Temperature cross sections (in colour) with overlaid isohalines...
• Figure 5. Results from backtracking in 2004 (left), 2005 (centre) and 2006...
• Figure 6. Temperature, salinity, and density profiles in the Gdask...

 
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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