Congelation ice is ice that forms on the bottom of an established ice cover.
Only the water freezes to ice, the salt from the seawater is concentrated into brine, some of which is contained in pockets in the new ice. Due to the brine pockets, congelation ice on seawater is neither as hard nor as transparent as fresh water ice.
On the surface of lakes, or other bodies of still freshwater, congelation ice is often called black Ice. This ice has frozen without many air bubbles trapped inside, making it transparent. Its transparency reveals the colour, usually black, of the water beneath it, hence the name. This is in contrast to snow ice, sometimes called slush ice, which is formed when slush (water saturated snow) refreezes. Snow ice is white due to the presence of air bubbles.
Black ice grows downward from the bottom of the existing ice surface. The growth rate of the ice is proportional to the rate that heat is transferred from the water below the ice surface to the air above the ice surface. The total ice thickness can be approximated from Stefan's equation.
- Sea Ice Types, Sea Ice Geophysics, University of Alaska
- National Snow and Ice Data Center: All About Sea Ice: Ice Formation Archived 2009-12-30 at the Wayback Machine.
- National Snow and Ice Data Center: All About Sea Ice: Salinity and Brine Archived 2009-12-18 at the Wayback Machine.
- LAKE ICE, from Alaska Lake Ice and Snow Observation Network
- The Acoustics of Thin Ice, by Gunnar Lundmark Archived 2008-12-04 at the Wayback Machine.
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