The East Greenland Polar Front in autumn

Closely spaced salinity and temperature measurements in the region of the East Greenland Polar Front from 75 N to 79 N in October-November 1981 are presented. The Return Atlantic Current (RAC), having a core of relatively warm and saline Atlantic Intermediate Water (AIW) (T = 0.5 to 3.0 C, S = 34.0...

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Main Authors: Paquette, Robert G., Bourke, Robert H., Newton, John L., Perdue, William F.
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 1985
Subjects:
Online Access:https://hdl.handle.net/10945/29257
id ftnavalpschool:oai:calhoun.nps.edu:10945/29257
record_format openpolar
spelling ftnavalpschool:oai:calhoun.nps.edu:10945/29257 2024-06-09T07:43:41+00:00 The East Greenland Polar Front in autumn Paquette, Robert G. Bourke, Robert H. Newton, John L. Perdue, William F. Operations Research (OR) Naval Postgraduate School (U.S.) Graduate School of Operational and Information Sciences (GSOIS) 1985-06 NA application/pdf https://hdl.handle.net/10945/29257 en_US eng Monterey, California. Naval Postgraduate School NPS-68-85-021 NA https://hdl.handle.net/10945/29257 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. East Greenland Current East Greenland Polar Front Fine structure NOKTHWIND Marginal Ice Zone Molloy Deep Eddy Greenland Sea Double-Diffusion FRONTS(OCEANOGRAPHY) Technical Report 1985 ftnavalpschool 2024-05-15T00:41:33Z Closely spaced salinity and temperature measurements in the region of the East Greenland Polar Front from 75 N to 79 N in October-November 1981 are presented. The Return Atlantic Current (RAC), having a core of relatively warm and saline Atlantic Intermediate Water (AIW) (T = 0.5 to 3.0 C, S = 34.0 to 35. 0), was found everywhere along a steep front separating it from the colder, fresher Polar Water. A narrow frontal jet was found to have velocities greater than 0.80 m/s where the station density was great enough to resolve its concentrated character. Notable fine structure was present, especially in the warm AIW just east of the front. A cold, saline water, forming a knee in the temperature-salinity correlation, was present in the upper margins of the RAC. The knee is formed primarily by warm AIW or Atlantic water flowing under the upper layers of water flowing form the Arctic Ocean. Calculations are presented to show that an initially isothermal underflow could be modified to a thick thermocline by double diffusion. Calculations of the rate of cooling of fine- structure elements by double diffusion indicate that the fine structure would have a limited lifetime (about 12 days) if its waters were not continually replenished supported in part by the Arctic Submarine Laboratory, Naval Ocean Systems Center, San Diego, CA under Work Order N 66001-84-WR00376. NA Prepared for: Director, Arctic Submarine Laboratory, Naval Ocean Systems Center http://archive.org/details/eastgreenlandpol00paqu Report Arctic Arctic Ocean Arctic Submarine Laboratory East Greenland east greenland current Greenland Greenland Sea Naval Postgraduate School: Calhoun Arctic Arctic Ocean Greenland Molloy ENVELOPE(70.065,70.065,-49.360,-49.360) Molloy Deep ENVELOPE(2.500,2.500,76.000,76.000)
institution Open Polar
collection Naval Postgraduate School: Calhoun
op_collection_id ftnavalpschool
language English
topic East Greenland Current
East Greenland Polar Front
Fine structure
NOKTHWIND
Marginal Ice Zone
Molloy Deep Eddy
Greenland Sea Double-Diffusion
FRONTS(OCEANOGRAPHY)
spellingShingle East Greenland Current
East Greenland Polar Front
Fine structure
NOKTHWIND
Marginal Ice Zone
Molloy Deep Eddy
Greenland Sea Double-Diffusion
FRONTS(OCEANOGRAPHY)
Paquette, Robert G.
Bourke, Robert H.
Newton, John L.
Perdue, William F.
The East Greenland Polar Front in autumn
topic_facet East Greenland Current
East Greenland Polar Front
Fine structure
NOKTHWIND
Marginal Ice Zone
Molloy Deep Eddy
Greenland Sea Double-Diffusion
FRONTS(OCEANOGRAPHY)
description Closely spaced salinity and temperature measurements in the region of the East Greenland Polar Front from 75 N to 79 N in October-November 1981 are presented. The Return Atlantic Current (RAC), having a core of relatively warm and saline Atlantic Intermediate Water (AIW) (T = 0.5 to 3.0 C, S = 34.0 to 35. 0), was found everywhere along a steep front separating it from the colder, fresher Polar Water. A narrow frontal jet was found to have velocities greater than 0.80 m/s where the station density was great enough to resolve its concentrated character. Notable fine structure was present, especially in the warm AIW just east of the front. A cold, saline water, forming a knee in the temperature-salinity correlation, was present in the upper margins of the RAC. The knee is formed primarily by warm AIW or Atlantic water flowing under the upper layers of water flowing form the Arctic Ocean. Calculations are presented to show that an initially isothermal underflow could be modified to a thick thermocline by double diffusion. Calculations of the rate of cooling of fine- structure elements by double diffusion indicate that the fine structure would have a limited lifetime (about 12 days) if its waters were not continually replenished supported in part by the Arctic Submarine Laboratory, Naval Ocean Systems Center, San Diego, CA under Work Order N 66001-84-WR00376. NA Prepared for: Director, Arctic Submarine Laboratory, Naval Ocean Systems Center http://archive.org/details/eastgreenlandpol00paqu
author2 Operations Research (OR)
Naval Postgraduate School (U.S.)
Graduate School of Operational and Information Sciences (GSOIS)
format Report
author Paquette, Robert G.
Bourke, Robert H.
Newton, John L.
Perdue, William F.
author_facet Paquette, Robert G.
Bourke, Robert H.
Newton, John L.
Perdue, William F.
author_sort Paquette, Robert G.
title The East Greenland Polar Front in autumn
title_short The East Greenland Polar Front in autumn
title_full The East Greenland Polar Front in autumn
title_fullStr The East Greenland Polar Front in autumn
title_full_unstemmed The East Greenland Polar Front in autumn
title_sort east greenland polar front in autumn
publisher Monterey, California. Naval Postgraduate School
publishDate 1985
url https://hdl.handle.net/10945/29257
long_lat ENVELOPE(70.065,70.065,-49.360,-49.360)
ENVELOPE(2.500,2.500,76.000,76.000)
geographic Arctic
Arctic Ocean
Greenland
Molloy
Molloy Deep
geographic_facet Arctic
Arctic Ocean
Greenland
Molloy
Molloy Deep
genre Arctic
Arctic Ocean
Arctic Submarine Laboratory
East Greenland
east greenland current
Greenland
Greenland Sea
genre_facet Arctic
Arctic Ocean
Arctic Submarine Laboratory
East Greenland
east greenland current
Greenland
Greenland Sea
op_relation NPS-68-85-021
NA
https://hdl.handle.net/10945/29257
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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