Finestructure, Fronts and Currents in the Pacific Marginal Sea-Ice Zone - MIZPAC 78.
Sharp vertical temperature fronts, complex temperature inversions and current patterns in the Chukchi Sea during MIZPAC 78 in July 1978 were investigated in a further effort to define the mechanisms for the formation and distribution of finestructure. In conformity with previous findings, upper and...
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ftdtic:ADA071970 2023-05-15T15:05:39+02:00 Finestructure, Fronts and Currents in the Pacific Marginal Sea-Ice Zone - MIZPAC 78. Small,Warren Edgar NAVAL POSTGRADUATE SCHOOL MONTEREY CA 1979-06 text/html http://www.dtic.mil/docs/citations/ADA071970 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA071970 en eng http://www.dtic.mil/docs/citations/ADA071970 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography Acoustics *OCEANOGRAPHIC DATA *UNDERWATER ACOUSTICS *SEA ICE TEMPERATURE OCEAN CURRENTS THESES SALINITY THERMOCLINES UPWELLING CHUKCHI SEA ARCTIC OCEAN MIZPAC 78 cruises USCGC glacier PE62759N Text 1979 ftdtic 2016-02-20T16:34:25Z Sharp vertical temperature fronts, complex temperature inversions and current patterns in the Chukchi Sea during MIZPAC 78 in July 1978 were investigated in a further effort to define the mechanisms for the formation and distribution of finestructure. In conformity with previous findings, upper and lower-layer fronts near the ice tended to be coincident in the V-shaped zones between bifurcating current streams; such fronts were not associated with significant finestructure. Previous thought would indicate that finestructure is found near wedge-like fronts. However, the situations for which this could be tested in 1978 were too few to be conclusive. Two of the principal ice embayments, which were apparently caused by warm water streams, were found in approximately the same locations as in previous years. Upper-level current streams, deduced from the ice melt-back into embayments and from warm-water cores, appear to be bathymetrically steered. Both of the above mentioned bays contain temperature finestructure. Text Arctic Arctic Ocean Chukchi Chukchi Sea Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Chukchi Sea Pacific |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Physical and Dynamic Oceanography Acoustics *OCEANOGRAPHIC DATA *UNDERWATER ACOUSTICS *SEA ICE TEMPERATURE OCEAN CURRENTS THESES SALINITY THERMOCLINES UPWELLING CHUKCHI SEA ARCTIC OCEAN MIZPAC 78 cruises USCGC glacier PE62759N |
spellingShingle |
Physical and Dynamic Oceanography Acoustics *OCEANOGRAPHIC DATA *UNDERWATER ACOUSTICS *SEA ICE TEMPERATURE OCEAN CURRENTS THESES SALINITY THERMOCLINES UPWELLING CHUKCHI SEA ARCTIC OCEAN MIZPAC 78 cruises USCGC glacier PE62759N Small,Warren Edgar Finestructure, Fronts and Currents in the Pacific Marginal Sea-Ice Zone - MIZPAC 78. |
topic_facet |
Physical and Dynamic Oceanography Acoustics *OCEANOGRAPHIC DATA *UNDERWATER ACOUSTICS *SEA ICE TEMPERATURE OCEAN CURRENTS THESES SALINITY THERMOCLINES UPWELLING CHUKCHI SEA ARCTIC OCEAN MIZPAC 78 cruises USCGC glacier PE62759N |
description |
Sharp vertical temperature fronts, complex temperature inversions and current patterns in the Chukchi Sea during MIZPAC 78 in July 1978 were investigated in a further effort to define the mechanisms for the formation and distribution of finestructure. In conformity with previous findings, upper and lower-layer fronts near the ice tended to be coincident in the V-shaped zones between bifurcating current streams; such fronts were not associated with significant finestructure. Previous thought would indicate that finestructure is found near wedge-like fronts. However, the situations for which this could be tested in 1978 were too few to be conclusive. Two of the principal ice embayments, which were apparently caused by warm water streams, were found in approximately the same locations as in previous years. Upper-level current streams, deduced from the ice melt-back into embayments and from warm-water cores, appear to be bathymetrically steered. Both of the above mentioned bays contain temperature finestructure. |
author2 |
NAVAL POSTGRADUATE SCHOOL MONTEREY CA |
format |
Text |
author |
Small,Warren Edgar |
author_facet |
Small,Warren Edgar |
author_sort |
Small,Warren Edgar |
title |
Finestructure, Fronts and Currents in the Pacific Marginal Sea-Ice Zone - MIZPAC 78. |
title_short |
Finestructure, Fronts and Currents in the Pacific Marginal Sea-Ice Zone - MIZPAC 78. |
title_full |
Finestructure, Fronts and Currents in the Pacific Marginal Sea-Ice Zone - MIZPAC 78. |
title_fullStr |
Finestructure, Fronts and Currents in the Pacific Marginal Sea-Ice Zone - MIZPAC 78. |
title_full_unstemmed |
Finestructure, Fronts and Currents in the Pacific Marginal Sea-Ice Zone - MIZPAC 78. |
title_sort |
finestructure, fronts and currents in the pacific marginal sea-ice zone - mizpac 78. |
publishDate |
1979 |
url |
http://www.dtic.mil/docs/citations/ADA071970 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA071970 |
geographic |
Arctic Arctic Ocean Chukchi Sea Pacific |
geographic_facet |
Arctic Arctic Ocean Chukchi Sea Pacific |
genre |
Arctic Arctic Ocean Chukchi Chukchi Sea Sea ice |
genre_facet |
Arctic Arctic Ocean Chukchi Chukchi Sea Sea ice |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA071970 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766337301860843520 |