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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Main Authors: Mcguinness Landman Trodahl, M. J. Mcguinness, K. A. Landman, H. J. Trodahl
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access: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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spelling 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
institution Open Polar
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language 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.
author2 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
geographic_facet Antarctic
genre Antarc*
Antarctic
Sea ice
genre_facet Antarc*
Antarctic
Sea ice
op_source http://www.mcs.vuw.ac.nz/math/papers/sun-on-sea-ice.ps
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http://www.mcs.vuw.ac.nz/math/papers/sun-on-sea-ice.ps
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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