OVIDE 2010 CTD-O2 Cruise report

The Ovide 5 cruise was carried out from the 7th of June to the 8th of July 2010 on board the N/O Thalassa. It was the fifth and last occurence of the Ovide hydrological section that was performed in June 2002, 2004, 2006, 2008, as part of the CLIVAR program under the name of A25. It is mainly funded...

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Main Authors: Branellec, Pierre, Thierry, Virginie
Format: Report
Language:English
Published: 2013
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00210/32134/30591.pdf
https://archimer.ifremer.fr/doc/00210/32134/
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spelling ftarchimer:oai:archimer.ifremer.fr:32134 2023-05-15T16:28:15+02:00 OVIDE 2010 CTD-O2 Cruise report Branellec, Pierre Thierry, Virginie 2013-01 application/pdf https://archimer.ifremer.fr/doc/00210/32134/30591.pdf https://archimer.ifremer.fr/doc/00210/32134/ eng eng https://archimer.ifremer.fr/doc/00210/32134/30591.pdf https://archimer.ifremer.fr/doc/00210/32134/ info:eu-repo/semantics/openAccess restricted use text Report info:eu-repo/semantics/report 2013 ftarchimer 2021-09-23T20:24:50Z The Ovide 5 cruise was carried out from the 7th of June to the 8th of July 2010 on board the N/O Thalassa. It was the fifth and last occurence of the Ovide hydrological section that was performed in June 2002, 2004, 2006, 2008, as part of the CLIVAR program under the name of A25. It is mainly funded by Ifremer, INSU (LEFE-IDAO) and UBO. The Ovide Principal Investigator is Herlé Mercier. A Greenland-Portugal section was previously performed in 1997 under the leadership of S. Bacon (NOCS), slighty south of the Ovide path. The Ovide route is redundant with AR7E (called also A1) on its western part. It begins at Cape Hoppe (southeast tip of Greenland), runs through the Irminger Sea, crosses the Reykjanes Ridge (300 miles north of Charlie-Gibbs Fracture Zone), runs through the Iceland Basin and the West European Basin (without having to sample on top of the complex Mid-Atlantic Ridge) and ends near Lisbon (Portugal). The objective of this repeated hydrological section is to monitor the variability of water mass properties and main current transports in the basin, complementing the international observation array relevant for climate studies. The hydrological section includes 98 surface-bottom stations from coast to coast, collecting profiles of temperature, salinity, oxygen and currents, spaced by 1 to 25 Nm depending on the steepness of the topography. In addition, three test stations and eleven stations in the Labrador Sea were performed. This report presents the results of the CTD-O2 data adjustment. Report Greenland Iceland Labrador Sea Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Greenland Irminger Sea ENVELOPE(-34.041,-34.041,63.054,63.054) Mid-Atlantic Ridge Reykjanes ENVELOPE(-22.250,-22.250,65.467,65.467) West European Basin ENVELOPE(-28.000,-28.000,52.750,52.750)
institution Open Polar
collection Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer)
op_collection_id ftarchimer
language English
description The Ovide 5 cruise was carried out from the 7th of June to the 8th of July 2010 on board the N/O Thalassa. It was the fifth and last occurence of the Ovide hydrological section that was performed in June 2002, 2004, 2006, 2008, as part of the CLIVAR program under the name of A25. It is mainly funded by Ifremer, INSU (LEFE-IDAO) and UBO. The Ovide Principal Investigator is Herlé Mercier. A Greenland-Portugal section was previously performed in 1997 under the leadership of S. Bacon (NOCS), slighty south of the Ovide path. The Ovide route is redundant with AR7E (called also A1) on its western part. It begins at Cape Hoppe (southeast tip of Greenland), runs through the Irminger Sea, crosses the Reykjanes Ridge (300 miles north of Charlie-Gibbs Fracture Zone), runs through the Iceland Basin and the West European Basin (without having to sample on top of the complex Mid-Atlantic Ridge) and ends near Lisbon (Portugal). The objective of this repeated hydrological section is to monitor the variability of water mass properties and main current transports in the basin, complementing the international observation array relevant for climate studies. The hydrological section includes 98 surface-bottom stations from coast to coast, collecting profiles of temperature, salinity, oxygen and currents, spaced by 1 to 25 Nm depending on the steepness of the topography. In addition, three test stations and eleven stations in the Labrador Sea were performed. This report presents the results of the CTD-O2 data adjustment.
format Report
author Branellec, Pierre
Thierry, Virginie
spellingShingle Branellec, Pierre
Thierry, Virginie
OVIDE 2010 CTD-O2 Cruise report
author_facet Branellec, Pierre
Thierry, Virginie
author_sort Branellec, Pierre
title OVIDE 2010 CTD-O2 Cruise report
title_short OVIDE 2010 CTD-O2 Cruise report
title_full OVIDE 2010 CTD-O2 Cruise report
title_fullStr OVIDE 2010 CTD-O2 Cruise report
title_full_unstemmed OVIDE 2010 CTD-O2 Cruise report
title_sort ovide 2010 ctd-o2 cruise report
publishDate 2013
url https://archimer.ifremer.fr/doc/00210/32134/30591.pdf
https://archimer.ifremer.fr/doc/00210/32134/
long_lat ENVELOPE(-34.041,-34.041,63.054,63.054)
ENVELOPE(-22.250,-22.250,65.467,65.467)
ENVELOPE(-28.000,-28.000,52.750,52.750)
geographic Greenland
Irminger Sea
Mid-Atlantic Ridge
Reykjanes
West European Basin
geographic_facet Greenland
Irminger Sea
Mid-Atlantic Ridge
Reykjanes
West European Basin
genre Greenland
Iceland
Labrador Sea
genre_facet Greenland
Iceland
Labrador Sea
op_relation https://archimer.ifremer.fr/doc/00210/32134/30591.pdf
https://archimer.ifremer.fr/doc/00210/32134/
op_rights info:eu-repo/semantics/openAccess
restricted use
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