A model of melt pond evolution on sea ice
[1] A one-dimensional, thermodynamic, and radiative model of a melt pond on sea ice is presented that explicitly treats the melt pond as an extra phase. A two-stream radiation model, which allows albedo to be determined from bulk optical properties, and a parameterization of the summertime evolution...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1046.6444 2023-05-15T18:16:33+02:00 A model of melt pond evolution on sea ice P D Taylor D L Feltham The Pennsylvania State University CiteSeerX Archives 2004 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1046.6444 http://centaur.reading.ac.uk/35289/1/Model%20of%20melt%20pond.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1046.6444 http://centaur.reading.ac.uk/35289/1/Model%20of%20melt%20pond.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://centaur.reading.ac.uk/35289/1/Model%20of%20melt%20pond.pdf text 2004 ftciteseerx 2020-04-05T00:19:55Z [1] A one-dimensional, thermodynamic, and radiative model of a melt pond on sea ice is presented that explicitly treats the melt pond as an extra phase. A two-stream radiation model, which allows albedo to be determined from bulk optical properties, and a parameterization of the summertime evolution of optical properties, is used. Heat transport within the sea ice is described using an equation describing heat transport in a mushy layer of a binary alloy (salt water). The model is tested by comparison of numerical simulations with SHEBA data and previous modeling. The presence of melt ponds on the sea ice surface is demonstrated to have a significant effect on the heat and mass balance. Sensitivity tests indicate that the maximum melt pond depth is highly sensitive to optical parameters and drainage. Text Sea ice Unknown |
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English |
description |
[1] A one-dimensional, thermodynamic, and radiative model of a melt pond on sea ice is presented that explicitly treats the melt pond as an extra phase. A two-stream radiation model, which allows albedo to be determined from bulk optical properties, and a parameterization of the summertime evolution of optical properties, is used. Heat transport within the sea ice is described using an equation describing heat transport in a mushy layer of a binary alloy (salt water). The model is tested by comparison of numerical simulations with SHEBA data and previous modeling. The presence of melt ponds on the sea ice surface is demonstrated to have a significant effect on the heat and mass balance. Sensitivity tests indicate that the maximum melt pond depth is highly sensitive to optical parameters and drainage. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
P D Taylor D L Feltham |
spellingShingle |
P D Taylor D L Feltham A model of melt pond evolution on sea ice |
author_facet |
P D Taylor D L Feltham |
author_sort |
P D Taylor |
title |
A model of melt pond evolution on sea ice |
title_short |
A model of melt pond evolution on sea ice |
title_full |
A model of melt pond evolution on sea ice |
title_fullStr |
A model of melt pond evolution on sea ice |
title_full_unstemmed |
A model of melt pond evolution on sea ice |
title_sort |
model of melt pond evolution on sea ice |
publishDate |
2004 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1046.6444 http://centaur.reading.ac.uk/35289/1/Model%20of%20melt%20pond.pdf |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
http://centaur.reading.ac.uk/35289/1/Model%20of%20melt%20pond.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1046.6444 http://centaur.reading.ac.uk/35289/1/Model%20of%20melt%20pond.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766190227093716992 |