RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 20, ES6005, doi:10.2205/2020ES000718, 2020

Figure 4. The model estimations of fast ice (solid lines) and mushy zone (dotted lines) thickness for a basin depth 0.5 (1), 1 (2) and 3 (3) m (a) and the freezing depth of water layers (1) and bottom sediments (2) as function of the basin depth (b) for the Winter 2015–2016 weather conditions. Zero in (a) corresponds to 3 November 2015.

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Citation: Bogorodskiy P. V., N. E. Demidov, K. V. Filchuk, A. V. Marchenko, E. G. Morozov, A. L. Nikulina, A. V. Pnyushkov, I. V. Ryzhov (2020), Growth of landfast ice and its thermal interaction with bottom sediments in the Braganzavägen Gulf (West Spitsbergen), Russ. J. Earth Sci., 20, ES6005, doi:10.2205/2020ES000718.

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