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Journal ArticleDOI

Some results from a time‐dependent thermodynamic model of sea ice

Gary A. Maykut, +1 more
- 20 Feb 1971 - 
- Vol. 76, Iss: 6, pp 1550-1575
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TLDR
In this paper, a one-dimensional thermodynamic model of sea ice is presented that includes the effects of snow cover, ice salinity, and internal heating due to penetration of solar radiation.
Abstract
A one-dimensional thermodynamic model of sea ice is presented that includes the effects of snow cover, ice salinity, and internal heating due to penetration of solar radiation. The incoming radiative and turbulent fluxes, oceanic heat flux, ice salinity, snow accumulation, and surface albedo are specified as functions of time. The model is applied to the central Arctic.

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Citations
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Journal ArticleDOI

Using sea ice to measure vertical heat flux in the ocean

TL;DR: In this paper, an experiment performed at drifting ice station FRAM I in the Arctic Ocean northwest of Spitzbergen during March-May 1979 indicate that sensible heat flux from the ocean to the ice cover was less than 2 W m−2.
Journal ArticleDOI

A Thickness and Enthalpy Distribution Sea-Ice Model

TL;DR: The theory of sea ice thickness distribution developed by Thorndike et al. as discussed by the authors has been extended to include sea ice enthalpy distribution, which conserves both ice mass and thermal energy, in the form of the heat stored in the ice.
Journal ArticleDOI

Arctic Sea ice decay simulated for a CO2-induced temperature rise

TL;DR: A large scale numerical time-dependent model of sea ice that takes into account the heat fluxes in and out of the ice, the seasonal occurrence of snow, and ice motions has been used in an experiment to determine the response of the Arctic Ocean ice pack to a warming of the atmosphere as discussed by the authors.
Journal ArticleDOI

The role of large‐scale under‐ice topography in separating estuary and ocean on an arctic shelf

TL;DR: In this paper, measurements of salinity and δ18O both from ice cores and the water column are used to infer the separation into two convective regimes due to the under-ice topography of the system of large pressure ridges that forms at the boundary between landfast ice and pack ice.
References
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Journal ArticleDOI

On the mass and heat budget of arctic sea ice

TL;DR: In this article, the authors show that during the summer seasons 1957 and 1958, an amount of 19.2 and 41.4 g/cm2 was lost by surface ablation on elevated dry surface and in meltwater ponds, respectively.
Journal ArticleDOI

Climate Through the Ages

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