Dmitrenko et al.: Oceanographic Causes for Transarctic Ice Transport
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Figure 8: The amount of heat transferred to the surface from the intermediate layer due to both convection at ice
formation (A) and double-diffusion convection (B), transect I of the Transdrift III expedition. A: I - by the time
the fast ice edge attains a quasi-steady character, II - by the time the ice growth ends, III - the total heat supply of
the intermediate water layer; B: I - by the time the fast ice edge attains a quasi-steady character (lower estimate),
II- the total heat supply of the intermediate water layer, III - the upper estimate of a potential transfer.