USNS BARTLETT Cruise to the Greenland Sea in September 1989: Data Report

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: Operations Research (OR), Naval Postgraduate School (U.S.), Graduate School of Operational and Information Sciences (GSOIS)
Format: Report
Language:English
Published: Monterey, California. Naval Postgraduate School 1990
Subjects:
Online Access:https://hdl.handle.net/10945/30276
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record_format openpolar
spelling ftnavalpschool:oai:calhoun.nps.edu:10945/30276 2024-06-09T07:44:09+00:00 USNS BARTLETT Cruise to the Greenland Sea in September 1989: Data Report Bourke, Robert H. Blythe, Robert F. Paquette, Robert G. Operations Research (OR) Naval Postgraduate School (U.S.) Graduate School of Operational and Information Sciences (GSOIS) 1990-07 application/pdf https://hdl.handle.net/10945/30276 en_US eng Monterey, California. Naval Postgraduate School NPS-68-90-006 https://hdl.handle.net/10945/30276 This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States. Greenland Sea Jan Mayen Current Greenland Sea Deep Water Norwegian Sea Deep Water Greenland Sea Project OCEAN CURRENTS Technical Report 1990 ftnavalpschool 2024-05-15T00:56:01Z 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 3000 m or more. Five north-south tending transects permitted tracking of the JMC by its low temperature (< 0°C) , low salinity near-surface core. The JMC could also be well defined from its warm, saline 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. O&MN, Direct Funding Arctic Submarine Laboratory, Naval Ocean Systems Center, San Diego, CA. http://archive.org/details/usnsbartlettcrui00bour Report Arctic Arctic Submarine Laboratory Greenland Greenland Sea Jan Mayen Norwegian Sea Naval Postgraduate School: Calhoun Arctic Greenland Jan Mayen Jan Mayen Fracture Zone ENVELOPE(-8.000,-8.000,71.200,71.200) Norwegian Sea
institution Open Polar
collection Naval Postgraduate School: Calhoun
op_collection_id ftnavalpschool
language English
topic Greenland Sea
Jan Mayen Current
Greenland Sea Deep Water
Norwegian Sea Deep Water
Greenland Sea Project
OCEAN CURRENTS
spellingShingle Greenland Sea
Jan Mayen Current
Greenland Sea Deep Water
Norwegian Sea Deep Water
Greenland Sea Project
OCEAN CURRENTS
Bourke, Robert H.
Blythe, Robert F.
Paquette, Robert G.
USNS BARTLETT Cruise to the Greenland Sea in September 1989: Data Report
topic_facet Greenland Sea
Jan Mayen Current
Greenland Sea Deep Water
Norwegian Sea Deep Water
Greenland Sea Project
OCEAN CURRENTS
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 3000 m or more. Five north-south tending transects permitted tracking of the JMC by its low temperature (< 0°C) , low salinity near-surface core. The JMC could also be well defined from its warm, saline 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. O&MN, Direct Funding Arctic Submarine Laboratory, Naval Ocean Systems Center, San Diego, CA. http://archive.org/details/usnsbartlettcrui00bour
author2 Operations Research (OR)
Naval Postgraduate School (U.S.)
Graduate School of Operational and Information Sciences (GSOIS)
format Report
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 USNS BARTLETT Cruise to the Greenland Sea in September 1989: Data Report
title_short USNS BARTLETT Cruise to the Greenland Sea in September 1989: Data Report
title_full USNS BARTLETT Cruise to the Greenland Sea in September 1989: Data Report
title_fullStr USNS BARTLETT Cruise to the Greenland Sea in September 1989: Data Report
title_full_unstemmed USNS BARTLETT Cruise to the Greenland Sea in September 1989: Data Report
title_sort usns bartlett cruise to the greenland sea in september 1989: data report
publisher Monterey, California. Naval Postgraduate School
publishDate 1990
url https://hdl.handle.net/10945/30276
long_lat ENVELOPE(-8.000,-8.000,71.200,71.200)
geographic Arctic
Greenland
Jan Mayen
Jan Mayen Fracture Zone
Norwegian Sea
geographic_facet Arctic
Greenland
Jan Mayen
Jan Mayen Fracture Zone
Norwegian Sea
genre Arctic
Arctic Submarine Laboratory
Greenland
Greenland Sea
Jan Mayen
Norwegian Sea
genre_facet Arctic
Arctic Submarine Laboratory
Greenland
Greenland Sea
Jan Mayen
Norwegian Sea
op_relation NPS-68-90-006
https://hdl.handle.net/10945/30276
op_rights This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.
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