Oceanographic Measurements in the Chukchi Sea and Baffin Bay - 1976
An oceanographic survey was conducted by helicopter in April 1976 in the ice-covered Chukchi Sea. This survey verified the existence of the bottom layer found a year earlier that had a temperature near the freezing point and a salinity relatively high for the Chukchi Sea. This bottom layer flows alo...
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ftdtic:ADA050225 2023-05-15T14:29:14+02:00 Oceanographic Measurements in the Chukchi Sea and Baffin Bay - 1976 Garrison,G R WASHINGTON UNIV SEATTLE APPLIED PHYSICS LAB 1977-10-15 text/html http://www.dtic.mil/docs/citations/ADA050225 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA050225 en eng http://www.dtic.mil/docs/citations/ADA050225 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography *OCEANOGRAPHIC DATA *CHUKCHI SEA *BAFFIN ISLAND TEMPERATURE ALASKA FREEZING SALINITY OCEANOGRAPHIC EQUIPMENT *Baffin Bay Barrow Canyon PE62759N WUMR01C2 Text 1977 ftdtic 2016-02-20T16:21:57Z An oceanographic survey was conducted by helicopter in April 1976 in the ice-covered Chukchi Sea. This survey verified the existence of the bottom layer found a year earlier that had a temperature near the freezing point and a salinity relatively high for the Chukchi Sea. This bottom layer flows along Alaska's northwest coast, through the Barrow Canyon, and into the Arctic Ocean. Its path is clearly visible in the vertical profiles of temperature and salinity taken at several lines of stations across the coastal zone. The flow down the Barrow Canyon is opposed by a westward spreading of the temperature-maximum layer of the western Arctic Basin and by an apparent uprising, or surge, of warm, saline Atlantic water from its usual depth of 140 m in the Arctic Ocean to a depth of 75 m. Similar conditions were observed in the spring of 1975. Some oceanographic measurements from an icebreaker were also conducted in Davis Strait and Baffin Bay during late February and March 1976. Temperature and salinity profiles revealed a deep, warm layer in Davis Strait which extended northward, with diminishing temperature, into Baffin Bay. (Author) Text Arctic Basin Arctic Arctic Ocean Baffin Bay Baffin Bay Baffin Island Baffin Barrow Chukchi Chukchi Sea Davis Strait Alaska Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Baffin Bay Baffin Island Barrow Canyon ENVELOPE(-154.000,-154.000,72.500,72.500) Chukchi Sea |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
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language |
English |
topic |
Physical and Dynamic Oceanography *OCEANOGRAPHIC DATA *CHUKCHI SEA *BAFFIN ISLAND TEMPERATURE ALASKA FREEZING SALINITY OCEANOGRAPHIC EQUIPMENT *Baffin Bay Barrow Canyon PE62759N WUMR01C2 |
spellingShingle |
Physical and Dynamic Oceanography *OCEANOGRAPHIC DATA *CHUKCHI SEA *BAFFIN ISLAND TEMPERATURE ALASKA FREEZING SALINITY OCEANOGRAPHIC EQUIPMENT *Baffin Bay Barrow Canyon PE62759N WUMR01C2 Garrison,G R Oceanographic Measurements in the Chukchi Sea and Baffin Bay - 1976 |
topic_facet |
Physical and Dynamic Oceanography *OCEANOGRAPHIC DATA *CHUKCHI SEA *BAFFIN ISLAND TEMPERATURE ALASKA FREEZING SALINITY OCEANOGRAPHIC EQUIPMENT *Baffin Bay Barrow Canyon PE62759N WUMR01C2 |
description |
An oceanographic survey was conducted by helicopter in April 1976 in the ice-covered Chukchi Sea. This survey verified the existence of the bottom layer found a year earlier that had a temperature near the freezing point and a salinity relatively high for the Chukchi Sea. This bottom layer flows along Alaska's northwest coast, through the Barrow Canyon, and into the Arctic Ocean. Its path is clearly visible in the vertical profiles of temperature and salinity taken at several lines of stations across the coastal zone. The flow down the Barrow Canyon is opposed by a westward spreading of the temperature-maximum layer of the western Arctic Basin and by an apparent uprising, or surge, of warm, saline Atlantic water from its usual depth of 140 m in the Arctic Ocean to a depth of 75 m. Similar conditions were observed in the spring of 1975. Some oceanographic measurements from an icebreaker were also conducted in Davis Strait and Baffin Bay during late February and March 1976. Temperature and salinity profiles revealed a deep, warm layer in Davis Strait which extended northward, with diminishing temperature, into Baffin Bay. (Author) |
author2 |
WASHINGTON UNIV SEATTLE APPLIED PHYSICS LAB |
format |
Text |
author |
Garrison,G R |
author_facet |
Garrison,G R |
author_sort |
Garrison,G R |
title |
Oceanographic Measurements in the Chukchi Sea and Baffin Bay - 1976 |
title_short |
Oceanographic Measurements in the Chukchi Sea and Baffin Bay - 1976 |
title_full |
Oceanographic Measurements in the Chukchi Sea and Baffin Bay - 1976 |
title_fullStr |
Oceanographic Measurements in the Chukchi Sea and Baffin Bay - 1976 |
title_full_unstemmed |
Oceanographic Measurements in the Chukchi Sea and Baffin Bay - 1976 |
title_sort |
oceanographic measurements in the chukchi sea and baffin bay - 1976 |
publishDate |
1977 |
url |
http://www.dtic.mil/docs/citations/ADA050225 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA050225 |
long_lat |
ENVELOPE(-154.000,-154.000,72.500,72.500) |
geographic |
Arctic Arctic Ocean Baffin Bay Baffin Island Barrow Canyon Chukchi Sea |
geographic_facet |
Arctic Arctic Ocean Baffin Bay Baffin Island Barrow Canyon Chukchi Sea |
genre |
Arctic Basin Arctic Arctic Ocean Baffin Bay Baffin Bay Baffin Island Baffin Barrow Chukchi Chukchi Sea Davis Strait Alaska |
genre_facet |
Arctic Basin Arctic Arctic Ocean Baffin Bay Baffin Bay Baffin Island Baffin Barrow Chukchi Chukchi Sea Davis Strait Alaska |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA050225 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766303296143753216 |