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

Figure 6. The model estimations of the rates of phase boundaries $w_i$ (1) and $w_m$ (2) for a 1 m basin depth (a) and the heat flux through the snow and ice cover (b) for a basin with a depth of 0.25 (1), 0.5 (2) and 1 (3) m. Zero time 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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