Solar Radiative Heating in First Year Sea Ice
Temperature measurements taken in young landfast Antarctic sea ice show daily oscillations consistent with heating by solar radiation. We present and solve a heat conduction model for the temperature with a nonlinear thermal capacity and a distributed source term for solar power absorption based on...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.7.4550 2023-05-15T13:31:12+02:00 Solar Radiative Heating in First Year Sea Ice Mcguinness Landman Trodahl M. J. Mcguinness K. A. Landman H. J. Trodahl The Pennsylvania State University CiteSeerX Archives application/postscript http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.7.4550 http://www.mcs.vuw.ac.nz/math/papers/sun-on-sea-ice.ps en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.7.4550 http://www.mcs.vuw.ac.nz/math/papers/sun-on-sea-ice.ps Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.mcs.vuw.ac.nz/math/papers/sun-on-sea-ice.ps text ftciteseerx 2016-01-08T18:49:41Z Temperature measurements taken in young landfast Antarctic sea ice show daily oscillations consistent with heating by solar radiation. We present and solve a heat conduction model for the temperature with a nonlinear thermal capacity and a distributed source term for solar power absorption based on Monte Carlo scattering simulations of penetrating photons. We observe two characteristic modes for solar heating in sea ice, one dominated by travelling thermal waves or conduction in the upper half, and the other dominated by in-place solar heating in the lower half. We note that deep thermal responses to solar radiation are larger by a factor of 10 than predicted by scattering measurements, due possibly to the presence of algae and/or dissolved organic material. Text Antarc* Antarctic Sea ice Unknown Antarctic |
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ftciteseerx |
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English |
description |
Temperature measurements taken in young landfast Antarctic sea ice show daily oscillations consistent with heating by solar radiation. We present and solve a heat conduction model for the temperature with a nonlinear thermal capacity and a distributed source term for solar power absorption based on Monte Carlo scattering simulations of penetrating photons. We observe two characteristic modes for solar heating in sea ice, one dominated by travelling thermal waves or conduction in the upper half, and the other dominated by in-place solar heating in the lower half. We note that deep thermal responses to solar radiation are larger by a factor of 10 than predicted by scattering measurements, due possibly to the presence of algae and/or dissolved organic material. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Mcguinness Landman Trodahl M. J. Mcguinness K. A. Landman H. J. Trodahl |
spellingShingle |
Mcguinness Landman Trodahl M. J. Mcguinness K. A. Landman H. J. Trodahl Solar Radiative Heating in First Year Sea Ice |
author_facet |
Mcguinness Landman Trodahl M. J. Mcguinness K. A. Landman H. J. Trodahl |
author_sort |
Mcguinness Landman Trodahl |
title |
Solar Radiative Heating in First Year Sea Ice |
title_short |
Solar Radiative Heating in First Year Sea Ice |
title_full |
Solar Radiative Heating in First Year Sea Ice |
title_fullStr |
Solar Radiative Heating in First Year Sea Ice |
title_full_unstemmed |
Solar Radiative Heating in First Year Sea Ice |
title_sort |
solar radiative heating in first year sea ice |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.7.4550 http://www.mcs.vuw.ac.nz/math/papers/sun-on-sea-ice.ps |
geographic |
Antarctic |
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Antarctic |
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Antarc* Antarctic Sea ice |
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Antarc* Antarctic Sea ice |
op_source |
http://www.mcs.vuw.ac.nz/math/papers/sun-on-sea-ice.ps |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.7.4550 http://www.mcs.vuw.ac.nz/math/papers/sun-on-sea-ice.ps |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766016633230327808 |