Numerical Simulation of Sea Ice Dynamics with the Discrete Element Method
This paper describes a discrete element model for sea ice dynamics. An ice field is modeled as a collection of circular ice particles that interact with each other and boundary walls. Geostrophic forces act as driving forces. Contacts are non-instantaneous and multiple contacts can occur simultaneou...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.488.8874 2023-05-15T18:16:58+02:00 Numerical Simulation of Sea Ice Dynamics with the Discrete Element Method Alexander Dorsk The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.488.8874 http://people.clarkson.edu/projects/reushen/reu_china/Website/assets/participants_assets/Reports/Bing.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.488.8874 http://people.clarkson.edu/projects/reushen/reu_china/Website/assets/participants_assets/Reports/Bing.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://people.clarkson.edu/projects/reushen/reu_china/Website/assets/participants_assets/Reports/Bing.pdf text ftciteseerx 2016-01-08T08:21:13Z This paper describes a discrete element model for sea ice dynamics. An ice field is modeled as a collection of circular ice particles that interact with each other and boundary walls. Geostrophic forces act as driving forces. Contacts are non-instantaneous and multiple contacts can occur simultaneously for each particle. Contact forces are modeled as viscous-elastic forces with a friction limit for the tangential component. Ridging effects were modeled by allowing particle size to vary when contact stress exceeds a plastic stress limit. Preliminary results for the model are reported. The results include a vortex wind field test, a unidirectional wind field test for ridging effects, and simulations of sea ice in the Bohai Sea. Text Sea ice Unknown |
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English |
description |
This paper describes a discrete element model for sea ice dynamics. An ice field is modeled as a collection of circular ice particles that interact with each other and boundary walls. Geostrophic forces act as driving forces. Contacts are non-instantaneous and multiple contacts can occur simultaneously for each particle. Contact forces are modeled as viscous-elastic forces with a friction limit for the tangential component. Ridging effects were modeled by allowing particle size to vary when contact stress exceeds a plastic stress limit. Preliminary results for the model are reported. The results include a vortex wind field test, a unidirectional wind field test for ridging effects, and simulations of sea ice in the Bohai Sea. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Alexander Dorsk |
spellingShingle |
Alexander Dorsk Numerical Simulation of Sea Ice Dynamics with the Discrete Element Method |
author_facet |
Alexander Dorsk |
author_sort |
Alexander Dorsk |
title |
Numerical Simulation of Sea Ice Dynamics with the Discrete Element Method |
title_short |
Numerical Simulation of Sea Ice Dynamics with the Discrete Element Method |
title_full |
Numerical Simulation of Sea Ice Dynamics with the Discrete Element Method |
title_fullStr |
Numerical Simulation of Sea Ice Dynamics with the Discrete Element Method |
title_full_unstemmed |
Numerical Simulation of Sea Ice Dynamics with the Discrete Element Method |
title_sort |
numerical simulation of sea ice dynamics with the discrete element method |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.488.8874 http://people.clarkson.edu/projects/reushen/reu_china/Website/assets/participants_assets/Reports/Bing.pdf |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
http://people.clarkson.edu/projects/reushen/reu_china/Website/assets/participants_assets/Reports/Bing.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.488.8874 http://people.clarkson.edu/projects/reushen/reu_china/Website/assets/participants_assets/Reports/Bing.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766190959430729728 |