“…Turning to another motivational aspect that determines the interest in the development of models with moving boundaries, we especially emphasize the importance of studying the effect of melt water percolating into the ice matrix, leading to a strong reduction in the surface salinity and bringing the requirements for the correspondent mathematical apparatus to the next level. When relatively low-salinity meltwater comes into the contact with oceanic waters each at or close to their respective freezing points [21][22][23], it can be retained under thin ice in bottom hollows, leading to double-diffusion at the interface between freshwater and seawater and consequent formation of "under-ice melt ponds" [1,2] also known as "false bottom effect" [1,2,21,24] (Figure 1). The false bottom effect is known as the only reliable source of ice formation during the polar summer [7,23,25], confirmed by both field and laboratory experiments [23,[25][26][27], as well as modeling studies [28,29]; it plays a critical role as a reservoir for meteoric water (snowmelt water) and in the transfer of atmospheric pollutants to the pack ice [30].…”