ON THE STEADY-STATE FLOW OF SEA ICE.
The purpose of this paper is to create a model in which the ice and ocean are viewed as a dynamic unit and in which the gradient currents and internal ice stresses are included. Also, this paper is concerned with the solution of such a model.
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1964
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ftdtic:AD0604368 2023-05-15T14:55:25+02:00 ON THE STEADY-STATE FLOW OF SEA ICE. Campbell,William Joseph WASHINGTON UNIV SEATTLE 1964-07 text/html http://www.dtic.mil/docs/citations/AD0604368 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0604368 en eng http://www.dtic.mil/docs/citations/AD0604368 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS *ARCTIC OCEAN OCEANS ICE ICE ISLANDS DRIFT OCEAN CURRENTS STRESSES MARINE GEOPHYSICS OCEANOGRAPHIC DATA MATHEMATICAL MODELS COMPUTER PROGRAMMING Text 1964 ftdtic 2016-02-21T16:36:49Z The purpose of this paper is to create a model in which the ice and ocean are viewed as a dynamic unit and in which the gradient currents and internal ice stresses are included. Also, this paper is concerned with the solution of such a model. Text Arctic Arctic Ocean Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
*ARCTIC OCEAN OCEANS ICE ICE ISLANDS DRIFT OCEAN CURRENTS STRESSES MARINE GEOPHYSICS OCEANOGRAPHIC DATA MATHEMATICAL MODELS COMPUTER PROGRAMMING |
spellingShingle |
*ARCTIC OCEAN OCEANS ICE ICE ISLANDS DRIFT OCEAN CURRENTS STRESSES MARINE GEOPHYSICS OCEANOGRAPHIC DATA MATHEMATICAL MODELS COMPUTER PROGRAMMING Campbell,William Joseph ON THE STEADY-STATE FLOW OF SEA ICE. |
topic_facet |
*ARCTIC OCEAN OCEANS ICE ICE ISLANDS DRIFT OCEAN CURRENTS STRESSES MARINE GEOPHYSICS OCEANOGRAPHIC DATA MATHEMATICAL MODELS COMPUTER PROGRAMMING |
description |
The purpose of this paper is to create a model in which the ice and ocean are viewed as a dynamic unit and in which the gradient currents and internal ice stresses are included. Also, this paper is concerned with the solution of such a model. |
author2 |
WASHINGTON UNIV SEATTLE |
format |
Text |
author |
Campbell,William Joseph |
author_facet |
Campbell,William Joseph |
author_sort |
Campbell,William Joseph |
title |
ON THE STEADY-STATE FLOW OF SEA ICE. |
title_short |
ON THE STEADY-STATE FLOW OF SEA ICE. |
title_full |
ON THE STEADY-STATE FLOW OF SEA ICE. |
title_fullStr |
ON THE STEADY-STATE FLOW OF SEA ICE. |
title_full_unstemmed |
ON THE STEADY-STATE FLOW OF SEA ICE. |
title_sort |
on the steady-state flow of sea ice. |
publishDate |
1964 |
url |
http://www.dtic.mil/docs/citations/AD0604368 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0604368 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Sea ice |
genre_facet |
Arctic Arctic Ocean Sea ice |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0604368 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766327304389132288 |