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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Bibliographic Details
Main Author: Garrison,G R
Other Authors: WASHINGTON UNIV SEATTLE APPLIED PHYSICS LAB
Format: Text
Language:English
Published: 1977
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA050225
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA050225
id ftdtic:ADA050225
record_format openpolar
spelling 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
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
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
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