ON THE EVALUATION OF ICE MODELS
Amethod is presented for an evaluation of coupled dynamic and thermodynamic ice models using the RADARSAT Geophysical Processor System (RGPS) data and prod-ucts for validation. The technique has been applied to a standard viscous-plastic rhe-ology with a simple two-level ice thickness model for thre...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.523.5735 2023-05-15T14:58:27+02:00 ON THE EVALUATION OF ICE MODELS D. Sulsky K. Peterson H. Schreyer R. Kwok M. Coon The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.523.5735 http://math.unm.edu/~sulsky/papers/SulskyPOAC05.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.523.5735 http://math.unm.edu/~sulsky/papers/SulskyPOAC05.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://math.unm.edu/~sulsky/papers/SulskyPOAC05.pdf text ftciteseerx 2016-01-08T10:15:20Z Amethod is presented for an evaluation of coupled dynamic and thermodynamic ice models using the RADARSAT Geophysical Processor System (RGPS) data and prod-ucts for validation. The technique has been applied to a standard viscous-plastic rhe-ology with a simple two-level ice thickness model for three test regions of the Arctic pack ice. High correlation is obtained between observed and predicted ice speeds. The model predictions show reasonable correlation with the data when examining shear and vorticity, but poorer correlation with divergence. The amount of opening is under pre-dicted in these simulations. Text Arctic Unknown Arctic |
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ftciteseerx |
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English |
description |
Amethod is presented for an evaluation of coupled dynamic and thermodynamic ice models using the RADARSAT Geophysical Processor System (RGPS) data and prod-ucts for validation. The technique has been applied to a standard viscous-plastic rhe-ology with a simple two-level ice thickness model for three test regions of the Arctic pack ice. High correlation is obtained between observed and predicted ice speeds. The model predictions show reasonable correlation with the data when examining shear and vorticity, but poorer correlation with divergence. The amount of opening is under pre-dicted in these simulations. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
D. Sulsky K. Peterson H. Schreyer R. Kwok M. Coon |
spellingShingle |
D. Sulsky K. Peterson H. Schreyer R. Kwok M. Coon ON THE EVALUATION OF ICE MODELS |
author_facet |
D. Sulsky K. Peterson H. Schreyer R. Kwok M. Coon |
author_sort |
D. Sulsky |
title |
ON THE EVALUATION OF ICE MODELS |
title_short |
ON THE EVALUATION OF ICE MODELS |
title_full |
ON THE EVALUATION OF ICE MODELS |
title_fullStr |
ON THE EVALUATION OF ICE MODELS |
title_full_unstemmed |
ON THE EVALUATION OF ICE MODELS |
title_sort |
on the evaluation of ice models |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.523.5735 http://math.unm.edu/~sulsky/papers/SulskyPOAC05.pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
http://math.unm.edu/~sulsky/papers/SulskyPOAC05.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.523.5735 http://math.unm.edu/~sulsky/papers/SulskyPOAC05.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766330560958955520 |