Oceanographic Observations, North Atlantic Ocean Station BRAVO Terminal Report 1964 - 1974
Observed and interpolated temperature and salinity data, plus computed sigma-t, geopotential anomalies, sound velocities and a limited number of dissolved oxygen values are presented for 1249 oceanographic stations taken by U.S. Coast Guard cutters at Ocean Station BRAVO (56 deg. 30'N, 51 deg....
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ftdtic:ADA112336 2023-05-15T17:30:23+02:00 Oceanographic Observations, North Atlantic Ocean Station BRAVO Terminal Report 1964 - 1974 Shuhy,J L COAST GUARD WASHINGTON DC OCEANOGRAPHIC UNIT 1978-09 text/html http://www.dtic.mil/docs/citations/ADA112336 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA112336 en eng http://www.dtic.mil/docs/citations/ADA112336 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography *Sea water Temperature Atmospheric temperature Oceanographic data Surface temperature Oxygen Ocean surface North Atlantic Ocean Deep water Ocean bottom Stratification Stations Salinity Density Surface waters Interpolation Time series analysis Cooling Ocean Station BRAVO Bottom water Dissolved oxygen Text 1978 ftdtic 2016-02-19T07:46:29Z Observed and interpolated temperature and salinity data, plus computed sigma-t, geopotential anomalies, sound velocities and a limited number of dissolved oxygen values are presented for 1249 oceanographic stations taken by U.S. Coast Guard cutters at Ocean Station BRAVO (56 deg. 30'N, 51 deg. 00'W) from November 1969 through June 1974. In addition, a time-series analysis of monthly averages of air and sea surface temperature, salinity, and sigma-t are presented for data collected at OS BRAVO since the inception of the oceanographic program in January 1964. This analysis reveals a five year cooling and freshening trend of the surface waters between 1967 and 1971 which resulted in a decrease in density of the surface waters. This decrease in density resulted in a stratification of the water column in the upper 200 meters inhibiting an overturn of the water column and the formation of deep and bottom waterin this area. (Author) Text North Atlantic Defense Technical Information Center: DTIC Technical Reports database |
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Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Physical and Dynamic Oceanography *Sea water Temperature Atmospheric temperature Oceanographic data Surface temperature Oxygen Ocean surface North Atlantic Ocean Deep water Ocean bottom Stratification Stations Salinity Density Surface waters Interpolation Time series analysis Cooling Ocean Station BRAVO Bottom water Dissolved oxygen |
spellingShingle |
Physical and Dynamic Oceanography *Sea water Temperature Atmospheric temperature Oceanographic data Surface temperature Oxygen Ocean surface North Atlantic Ocean Deep water Ocean bottom Stratification Stations Salinity Density Surface waters Interpolation Time series analysis Cooling Ocean Station BRAVO Bottom water Dissolved oxygen Shuhy,J L Oceanographic Observations, North Atlantic Ocean Station BRAVO Terminal Report 1964 - 1974 |
topic_facet |
Physical and Dynamic Oceanography *Sea water Temperature Atmospheric temperature Oceanographic data Surface temperature Oxygen Ocean surface North Atlantic Ocean Deep water Ocean bottom Stratification Stations Salinity Density Surface waters Interpolation Time series analysis Cooling Ocean Station BRAVO Bottom water Dissolved oxygen |
description |
Observed and interpolated temperature and salinity data, plus computed sigma-t, geopotential anomalies, sound velocities and a limited number of dissolved oxygen values are presented for 1249 oceanographic stations taken by U.S. Coast Guard cutters at Ocean Station BRAVO (56 deg. 30'N, 51 deg. 00'W) from November 1969 through June 1974. In addition, a time-series analysis of monthly averages of air and sea surface temperature, salinity, and sigma-t are presented for data collected at OS BRAVO since the inception of the oceanographic program in January 1964. This analysis reveals a five year cooling and freshening trend of the surface waters between 1967 and 1971 which resulted in a decrease in density of the surface waters. This decrease in density resulted in a stratification of the water column in the upper 200 meters inhibiting an overturn of the water column and the formation of deep and bottom waterin this area. (Author) |
author2 |
COAST GUARD WASHINGTON DC OCEANOGRAPHIC UNIT |
format |
Text |
author |
Shuhy,J L |
author_facet |
Shuhy,J L |
author_sort |
Shuhy,J L |
title |
Oceanographic Observations, North Atlantic Ocean Station BRAVO Terminal Report 1964 - 1974 |
title_short |
Oceanographic Observations, North Atlantic Ocean Station BRAVO Terminal Report 1964 - 1974 |
title_full |
Oceanographic Observations, North Atlantic Ocean Station BRAVO Terminal Report 1964 - 1974 |
title_fullStr |
Oceanographic Observations, North Atlantic Ocean Station BRAVO Terminal Report 1964 - 1974 |
title_full_unstemmed |
Oceanographic Observations, North Atlantic Ocean Station BRAVO Terminal Report 1964 - 1974 |
title_sort |
oceanographic observations, north atlantic ocean station bravo terminal report 1964 - 1974 |
publishDate |
1978 |
url |
http://www.dtic.mil/docs/citations/ADA112336 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA112336 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA112336 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766126765923631104 |