Preliminary Cruise Report of USNS Bartlett to the Greenland Sea in September 1989

As a component of the Greenland Sea Project, a hydrographic cruise was conducted on board the USNS BARTLETT during September 1989 in the southern Greenland Sea to characterize the water mass structure and circulation features of the Jan Mayen Current (JMC). A total of 48 high-quality CTD stations we...

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Main Authors: Bourke, Robert H., Blythe, Robert F., Paquette, Robert G.
Other Authors: NAVAL POSTGRADUATE SCHOOL MONTEREY CA
Format: Text
Language:English
Published: 1989
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA218074
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA218074
id ftdtic:ADA218074
record_format openpolar
spelling ftdtic:ADA218074 2023-05-15T16:23:16+02:00 Preliminary Cruise Report of USNS Bartlett to the Greenland Sea in September 1989 Bourke, Robert H. Blythe, Robert F. Paquette, Robert G. NAVAL POSTGRADUATE SCHOOL MONTEREY CA 1989-12 text/html http://www.dtic.mil/docs/citations/ADA218074 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA218074 en eng http://www.dtic.mil/docs/citations/ADA218074 Approved for public release; distribution is unlimited. DTIC AND NTIS Hydrology Limnology and Potamology *HYDROGRAPHY GREENLAND CORES PHYSICAL PROPERTIES WATER TRACKING FRACTURE(MECHANICS) SALINITY NORWEGIAN SEA WATER MASSES DEEP WATER BOTTOM SOUTH(DIRECTION) GREENLAND SEA STATIONS LOW TEMPERATURE Text 1989 ftdtic 2016-02-23T02:28:05Z As a component of the Greenland Sea Project, a hydrographic cruise was conducted on board the USNS BARTLETT during September 1989 in the southern Greenland Sea to characterize the water mass structure and circulation features of the Jan Mayen Current (JMC). A total of 48 high-quality CTD stations were occupied to depths of 1000 m; five stations extended to 3000m or more. Five north-south tending transects permitted tracking of the JMC by its low temperature (< 0 deg C), low salinity core. The JMC could also be well defined from its intermediate water properties. Deep stations made in the trough of the Jan Mayen Fracture Zone suggest that the interchange of deep and bottom water from the Greenland and Norwegian Seas via this trough is a slow diffusive process and not an active advective feature as previously thought. Keywords: Greenland sea, Jan mayen current, Greenland sea deep water, Norwegian sea deep water, Greenland sea project. Text Greenland Greenland Sea Jan Mayen Norwegian Sea Defense Technical Information Center: DTIC Technical Reports database Greenland Jan Mayen Jan Mayen Fracture Zone ENVELOPE(-8.000,-8.000,71.200,71.200) Norwegian Sea
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Hydrology
Limnology and Potamology
*HYDROGRAPHY
GREENLAND
CORES
PHYSICAL PROPERTIES
WATER
TRACKING
FRACTURE(MECHANICS)
SALINITY
NORWEGIAN SEA
WATER MASSES
DEEP WATER
BOTTOM
SOUTH(DIRECTION)
GREENLAND SEA
STATIONS
LOW TEMPERATURE
spellingShingle Hydrology
Limnology and Potamology
*HYDROGRAPHY
GREENLAND
CORES
PHYSICAL PROPERTIES
WATER
TRACKING
FRACTURE(MECHANICS)
SALINITY
NORWEGIAN SEA
WATER MASSES
DEEP WATER
BOTTOM
SOUTH(DIRECTION)
GREENLAND SEA
STATIONS
LOW TEMPERATURE
Bourke, Robert H.
Blythe, Robert F.
Paquette, Robert G.
Preliminary Cruise Report of USNS Bartlett to the Greenland Sea in September 1989
topic_facet Hydrology
Limnology and Potamology
*HYDROGRAPHY
GREENLAND
CORES
PHYSICAL PROPERTIES
WATER
TRACKING
FRACTURE(MECHANICS)
SALINITY
NORWEGIAN SEA
WATER MASSES
DEEP WATER
BOTTOM
SOUTH(DIRECTION)
GREENLAND SEA
STATIONS
LOW TEMPERATURE
description As a component of the Greenland Sea Project, a hydrographic cruise was conducted on board the USNS BARTLETT during September 1989 in the southern Greenland Sea to characterize the water mass structure and circulation features of the Jan Mayen Current (JMC). A total of 48 high-quality CTD stations were occupied to depths of 1000 m; five stations extended to 3000m or more. Five north-south tending transects permitted tracking of the JMC by its low temperature (< 0 deg C), low salinity core. The JMC could also be well defined from its intermediate water properties. Deep stations made in the trough of the Jan Mayen Fracture Zone suggest that the interchange of deep and bottom water from the Greenland and Norwegian Seas via this trough is a slow diffusive process and not an active advective feature as previously thought. Keywords: Greenland sea, Jan mayen current, Greenland sea deep water, Norwegian sea deep water, Greenland sea project.
author2 NAVAL POSTGRADUATE SCHOOL MONTEREY CA
format Text
author Bourke, Robert H.
Blythe, Robert F.
Paquette, Robert G.
author_facet Bourke, Robert H.
Blythe, Robert F.
Paquette, Robert G.
author_sort Bourke, Robert H.
title Preliminary Cruise Report of USNS Bartlett to the Greenland Sea in September 1989
title_short Preliminary Cruise Report of USNS Bartlett to the Greenland Sea in September 1989
title_full Preliminary Cruise Report of USNS Bartlett to the Greenland Sea in September 1989
title_fullStr Preliminary Cruise Report of USNS Bartlett to the Greenland Sea in September 1989
title_full_unstemmed Preliminary Cruise Report of USNS Bartlett to the Greenland Sea in September 1989
title_sort preliminary cruise report of usns bartlett to the greenland sea in september 1989
publishDate 1989
url http://www.dtic.mil/docs/citations/ADA218074
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA218074
long_lat ENVELOPE(-8.000,-8.000,71.200,71.200)
geographic Greenland
Jan Mayen
Jan Mayen Fracture Zone
Norwegian Sea
geographic_facet Greenland
Jan Mayen
Jan Mayen Fracture Zone
Norwegian Sea
genre Greenland
Greenland Sea
Jan Mayen
Norwegian Sea
genre_facet Greenland
Greenland Sea
Jan Mayen
Norwegian Sea
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA218074
op_rights Approved for public release; distribution is unlimited.
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