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Examples
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Competing marine users in newly open or partially icecovered areas in the Arctic are likely to require increased enforcement presence and regulatory oversight.
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Processes specific to the surface boundary layer include the radically different surface fluxes in icecovered versus ice-free fractions of a climate model grid cell; the strongly asymmetrical behavior of ice basal melting versus freezing; the interaction of morphology and wave with ice-bottom climate model; and the modification of momentum transfer mechanisms as surface stochastic analysis effects are replaced by stress transfer through the sea ice cover.
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Most of the Arctic Ocean is projected to remain icecovered in March, although the March sea ice edge is projected to retreat substantially in the subpolar seas.
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'There may be no need,' said Taliesen softly, pointing to the icecovered pool.
Ironhand's Daughter Gemmell, David 1995
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Processes specific to the surface boundary layer include the radically different surface fluxes in icecovered versus ice-free fractions of a climate model grid cell; the strongly asymmetrical behavior of ice basal melting versus freezing; the interaction of morphology and wave with ice-bottom climate model; and the modification of momentum transfer mechanisms as surface stochastic analysis effects are replaced by stress transfer through the sea ice cover.
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Most of the Arctic Ocean is projected to remain icecovered in March, although the March sea ice edge is projected to retreat substantially in the subpolar seas.
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Most of the Arctic Ocean is projected to remain icecovered in March, although the March sea ice edge is projected to retreat substantially in the subpolar seas.
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Processes specific to the surface boundary layer include the radically different surface fluxes in icecovered versus ice-free fractions of a climate model grid cell; the strongly asymmetrical behavior of ice basal melting versus freezing; the interaction of morphology and wave with ice-bottom climate model; and the modification of momentum transfer mechanisms as surface stochastic analysis effects are replaced by stress transfer through the sea ice cover.
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