High Resolution Profiler Study of Deep Mixing in the Romanche Fracture Zone.

Between November 20 and December 10, 1994, studies of the deep mixing processes in the Romanche Fracture Zone (RFZ) of the Mid-Atlantic Ridge were conducted from the French research vessel N/O le Noroit. Oceanographers from France and the U.S. worked together to acquire the unique data obtained on t...

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Main Author: Montgomery, Ellyn T.
Other Authors: WOODS HOLE OCEANOGRAPHIC INSTITUTION MA
Format: Text
Language:English
Published: 1996
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA320898
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA320898
id ftdtic:ADA320898
record_format openpolar
spelling ftdtic:ADA320898 2023-05-15T13:50:52+02:00 High Resolution Profiler Study of Deep Mixing in the Romanche Fracture Zone. Montgomery, Ellyn T. WOODS HOLE OCEANOGRAPHIC INSTITUTION MA 1996-10 text/html http://www.dtic.mil/docs/citations/ADA320898 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA320898 en eng http://www.dtic.mil/docs/citations/ADA320898 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Geology Geochemistry and Mineralogy *FAULTS(GEOLOGY) *HYDROGRAPHIC SURVEYING *OCEAN RIDGES PROFILES SEDIMENTS RESEARCH SHIPS BOTTOM WATERS LE NOROIL VESSEL Text 1996 ftdtic 2016-02-19T19:30:40Z Between November 20 and December 10, 1994, studies of the deep mixing processes in the Romanche Fracture Zone (RFZ) of the Mid-Atlantic Ridge were conducted from the French research vessel N/O le Noroit. Oceanographers from France and the U.S. worked together to acquire the unique data obtained on this expedition. The cruise departed from and returned to Dakar, Senegal. Prior to the work in the RFZ, a sediment trap was recovered and returned to port. Two HRP engineering test dives were completed on the way to the fracture zone. The next week and a half was spent profiling with the HRP and CTD along the channel of the RFZ to identify regions of especially intense mixing. After that, two trans-equatorial sections were done with the HRP to examine the structure and intensity of the equatorial jets. The presence of bottom intensified flow to the east along the RFZ and enhanced mixing of Antarctic Bottom Water were both observed. Based on the measurements obtained during this experiment, transport through the RFZ is estimated to be 1 Sv. The work at sea, instrumentation, data return and some preliminary results are presented in this report. Text Antarc* Antarctic Defense Technical Information Center: DTIC Technical Reports database Antarctic Mid-Atlantic Ridge
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Geology
Geochemistry and Mineralogy
*FAULTS(GEOLOGY)
*HYDROGRAPHIC SURVEYING
*OCEAN RIDGES
PROFILES
SEDIMENTS
RESEARCH SHIPS
BOTTOM WATERS
LE NOROIL VESSEL
spellingShingle Geology
Geochemistry and Mineralogy
*FAULTS(GEOLOGY)
*HYDROGRAPHIC SURVEYING
*OCEAN RIDGES
PROFILES
SEDIMENTS
RESEARCH SHIPS
BOTTOM WATERS
LE NOROIL VESSEL
Montgomery, Ellyn T.
High Resolution Profiler Study of Deep Mixing in the Romanche Fracture Zone.
topic_facet Geology
Geochemistry and Mineralogy
*FAULTS(GEOLOGY)
*HYDROGRAPHIC SURVEYING
*OCEAN RIDGES
PROFILES
SEDIMENTS
RESEARCH SHIPS
BOTTOM WATERS
LE NOROIL VESSEL
description Between November 20 and December 10, 1994, studies of the deep mixing processes in the Romanche Fracture Zone (RFZ) of the Mid-Atlantic Ridge were conducted from the French research vessel N/O le Noroit. Oceanographers from France and the U.S. worked together to acquire the unique data obtained on this expedition. The cruise departed from and returned to Dakar, Senegal. Prior to the work in the RFZ, a sediment trap was recovered and returned to port. Two HRP engineering test dives were completed on the way to the fracture zone. The next week and a half was spent profiling with the HRP and CTD along the channel of the RFZ to identify regions of especially intense mixing. After that, two trans-equatorial sections were done with the HRP to examine the structure and intensity of the equatorial jets. The presence of bottom intensified flow to the east along the RFZ and enhanced mixing of Antarctic Bottom Water were both observed. Based on the measurements obtained during this experiment, transport through the RFZ is estimated to be 1 Sv. The work at sea, instrumentation, data return and some preliminary results are presented in this report.
author2 WOODS HOLE OCEANOGRAPHIC INSTITUTION MA
format Text
author Montgomery, Ellyn T.
author_facet Montgomery, Ellyn T.
author_sort Montgomery, Ellyn T.
title High Resolution Profiler Study of Deep Mixing in the Romanche Fracture Zone.
title_short High Resolution Profiler Study of Deep Mixing in the Romanche Fracture Zone.
title_full High Resolution Profiler Study of Deep Mixing in the Romanche Fracture Zone.
title_fullStr High Resolution Profiler Study of Deep Mixing in the Romanche Fracture Zone.
title_full_unstemmed High Resolution Profiler Study of Deep Mixing in the Romanche Fracture Zone.
title_sort high resolution profiler study of deep mixing in the romanche fracture zone.
publishDate 1996
url http://www.dtic.mil/docs/citations/ADA320898
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA320898
geographic Antarctic
Mid-Atlantic Ridge
geographic_facet Antarctic
Mid-Atlantic Ridge
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA320898
op_rights APPROVED FOR PUBLIC RELEASE
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