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A Dynamic Thermodynamic Sea Ice Model
Journal of Physical Oceanography, 1979Abstract A numerical model for the simulation of sea ice circulation and thickness over a seasonal cycle is presented. This model is used to investigate the effects of ice dynamics on Arctic ice thickness and air-sea heat flux characteristics by carrying out several numerical simulations over the entire Arctic Ocean region.
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Nitrogen dynamics in a marginal sea-ice zone
Continental Shelf Research, 1987Abstract Intense blooms of phytoplankton develop at the edge of the seasonal sea ice in the southeastern Bering Sea in spring. These blooms are closely associated with extremely strong water column density stratification due to ice melt. Here we examine the nitrogen requirements of the phytoplankton and evaluate the importance of nitrogen sources to ...
Muller-Karger, Frank E, Alexander, V.
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Constitutive Laws for Sea Ice Dynamics Models
1997Abstract : The long term goal of my research is to develop sea ice dynamics models that describe behavior on kilometer scales and larger, and to base these models on the smaller scale physical processes known to control leading, rafting, and ridging. Three objectives were (1) to continue development of the new anisotropic plasticity constitutive law ...
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A 2-DIMENSIONAL MODEL FOR THE DYNAMICS OF SEA-ICE
Royal Society of London. Proceedings A. Mathematical, Physical and Engineering Sciences, 1994This paper develops a systematic analysis of a sea ice pack viewed as a thin layer of coherent ice floes and open water regions at the ocean surface. The pack is driven by wind stress and Coriolis force, with responsive water drag on the base of the floes.
Gray, Nico; id_orcid 0000-0003-3554-0499 +2 more
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Varying Response of Vegetation to Sea Ice Dynamics Over the Arctic
Science of the Total Environment, 2021Guoyong Leng, André Python
exaly
Investigations of Sea Ice Dynamics in the Baltic Sea
2001The Baltic Sea is a semi-enclosed basin in the seasonal sea ice zone. This ice dynamics problem offers its own particular regime of spatial scales below the large polar seas: the horizontal size of the basins is 100–300 km, the thickness of undeformed ice is up to 1 m, and ice ridges are typically 5–15 m thick.
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