Thickening ice tends to increase its longevity and its albedo (reflectiveness), both of which cool the planet. Pumping seawater onto sea ice may also brighten surfaces darkened by the deposition of soot, dust or organisms.

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Ice Thickening
Short DescriptionThickening ice tends to increase its longevity and its albedo (reflectiveness), both of which cool the planet. Pumping seawater onto sea ice may also brighten surfaces darkened by the deposition of soot, dust or organisms.
DescriptionAs ice thickens typically from its base, and ice is itself a good insulator, sea ice thickening rapidly tails off as the ice thickens. The thickening rate can be increased if water or seawater is pumped onto existing ice, and is therefore in contact with the typically much colder atmosphere and is further increased by wind chill. As brine freezes at a lower temperature than does seawater, the freezing rate can be increased still further: by allowing a rejected portion of brine to flow off a conical ice surface back into the sea; by using intermittent pumping; and by engineering only a shallow depth of pumped seawater.
MethodsEffectsProjects
Ice Shields/ISA
Arctic refreeze and GHG suppression
Irrigation
Reduce atmospheric methane concentrations in summer
Hazard of ice dam collapse
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In colder seasons, sea ice can be thickened by pumping seawater onto it in calibrated gushes so that it: forms semi-permanent, above and below ice polar habitat; enhances albedo; may stably ground the new ice arrays; stabilises coastlines, glaciers and the polar vortex; reduces or converts ebullient methane emissions; increases snowfall and off-planet heat radiation; and sequesters carbon dioxide and oxygen gases in the deep.
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