Freezing of Tidal Current Under Ice in a Shallow Channel
Аннотация и ключевые слова
Аннотация (русский):
We analyze tidal currents under ice in a shallow channel located near the tip of the Van Mijen Fjord in Spitsbergen. During the flood cycle of tide seawater flows under ice and strongly freezes in a shallow channel. During the ebb cycle salinity of the outflowing water is greater than that of the inflowing water. Salt balance is estimated. During high-water tide, salt water seeps through the cracks in the ice to the surface, which increases salinity of the snow and water mixture.

Ключевые слова:
Spitsbergen, shallow water, channel under ice, tidal current, freezing of seawater, salinity increase
Текст
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Список литературы

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