The dissolved salts in seawater increases the freezing point, explaining the formation of sea ice.

Name: The dissolved salts in seawater increases the freezing point, explaining the formation of sea ice.
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The freezing point of seawater is lowered with the increase of salinity. This makes it possible for seawater to form ice at lower temperatures than in freshwater. Information can be found in the section Seawater Consists of Water and Dissolved Solids.

The Dissolved Salts in Seawater Increases the Freezing Point, Explaining