Cruise 64PE400: Hydrographic survey of the Irminger Sea in July 2015 for the Overturning in the Subpolar North Atlantic Program (OSNAP) ...

During cruise 64PE400 the OSNAP East moorings, which were deployed in the Irminger Basin in summer 2014 have been recovered, serviced and redeployed. There are 5 moorings in the eastern Irminger Sea in the Irminger Current (IC) maintained by NIOZ, 5 moorings in the Western Irminger Sea in the Deep W...

Full description

Bibliographic Details
Main Authors: De Jong, Marieke, De Steur, Laura
Format: Dataset
Language:unknown
Published: SEANOE 2019
Subjects:
CTD
Online Access:https://dx.doi.org/10.17882/59302
https://www.seanoe.org/data/00481/59302/
id ftdatacite:10.17882/59302
record_format openpolar
spelling ftdatacite:10.17882/59302 2024-04-28T08:17:25+00:00 Cruise 64PE400: Hydrographic survey of the Irminger Sea in July 2015 for the Overturning in the Subpolar North Atlantic Program (OSNAP) ... De Jong, Marieke De Steur, Laura 2019 https://dx.doi.org/10.17882/59302 https://www.seanoe.org/data/00481/59302/ unknown SEANOE https://dx.doi.org/10.4121/uuid:77b2c4fc-c253-4494-91bd-8d1ef66a014a https://dx.doi.org/10.4121/uuid:9ae97ceb-39e4-43ec-abdb-614103285c16 https://dx.doi.org/10.1029/2023gl106501 https://dx.doi.org/10.1029/2020jc016193 https://dx.doi.org/10.1029/2018jc014730 https://dx.doi.org/10.1126/science.aau6592 https://dx.doi.org/10.1175/bams-d-16-0057.1 https://dx.doi.org/10.1002/2016gl069596 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CTD Irminger Sea hydrography OSNAP Pelagia 64PE400 dataset Dataset 2019 ftdatacite https://doi.org/10.17882/5930210.4121/uuid:77b2c4fc-c253-4494-91bd-8d1ef66a014a10.4121/uuid:9ae97ceb-39e4-43ec-abdb-614103285c1610.1029/2023gl10650110.1029/2020jc01619310.1029/2018jc01473010.1126/science.aau659210.1175/bams-d-16-0057.110.1002/2016gl069596 2024-04-02T10:44:55Z During cruise 64PE400 the OSNAP East moorings, which were deployed in the Irminger Basin in summer 2014 have been recovered, serviced and redeployed. There are 5 moorings in the eastern Irminger Sea in the Irminger Current (IC) maintained by NIOZ, 5 moorings in the Western Irminger Sea in the Deep Western Boundary Current (DWBC) maintained by NOC, and one mooring (LOCO2) in the centre of the Irminger gyre (section 4) maintained by NIOZ. A total of 34 RAFOS floats were released at target depths between 1800 and 2200 m in the eastern and western Irminger Sea as part of the US OSNAP program (see cruise report). The mooring work was complemented with repeat CTD stations on the former WOCE (or current CLIVAR) AR7E repeat section (between roughly 59°N, 31°W and 60°N, 42.5°W) including sampling for salinity and dissolved oxygen (O2) calibration. On the westernmost CTD stations in the East Greenland Current samples for ∂18O and nutrients were also taken.A second short CTD section was carried out on the Greenland ... Dataset East Greenland east greenland current Greenland North Atlantic DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic CTD
Irminger Sea
hydrography
OSNAP
Pelagia
64PE400
spellingShingle CTD
Irminger Sea
hydrography
OSNAP
Pelagia
64PE400
De Jong, Marieke
De Steur, Laura
Cruise 64PE400: Hydrographic survey of the Irminger Sea in July 2015 for the Overturning in the Subpolar North Atlantic Program (OSNAP) ...
topic_facet CTD
Irminger Sea
hydrography
OSNAP
Pelagia
64PE400
description During cruise 64PE400 the OSNAP East moorings, which were deployed in the Irminger Basin in summer 2014 have been recovered, serviced and redeployed. There are 5 moorings in the eastern Irminger Sea in the Irminger Current (IC) maintained by NIOZ, 5 moorings in the Western Irminger Sea in the Deep Western Boundary Current (DWBC) maintained by NOC, and one mooring (LOCO2) in the centre of the Irminger gyre (section 4) maintained by NIOZ. A total of 34 RAFOS floats were released at target depths between 1800 and 2200 m in the eastern and western Irminger Sea as part of the US OSNAP program (see cruise report). The mooring work was complemented with repeat CTD stations on the former WOCE (or current CLIVAR) AR7E repeat section (between roughly 59°N, 31°W and 60°N, 42.5°W) including sampling for salinity and dissolved oxygen (O2) calibration. On the westernmost CTD stations in the East Greenland Current samples for ∂18O and nutrients were also taken.A second short CTD section was carried out on the Greenland ...
format Dataset
author De Jong, Marieke
De Steur, Laura
author_facet De Jong, Marieke
De Steur, Laura
author_sort De Jong, Marieke
title Cruise 64PE400: Hydrographic survey of the Irminger Sea in July 2015 for the Overturning in the Subpolar North Atlantic Program (OSNAP) ...
title_short Cruise 64PE400: Hydrographic survey of the Irminger Sea in July 2015 for the Overturning in the Subpolar North Atlantic Program (OSNAP) ...
title_full Cruise 64PE400: Hydrographic survey of the Irminger Sea in July 2015 for the Overturning in the Subpolar North Atlantic Program (OSNAP) ...
title_fullStr Cruise 64PE400: Hydrographic survey of the Irminger Sea in July 2015 for the Overturning in the Subpolar North Atlantic Program (OSNAP) ...
title_full_unstemmed Cruise 64PE400: Hydrographic survey of the Irminger Sea in July 2015 for the Overturning in the Subpolar North Atlantic Program (OSNAP) ...
title_sort cruise 64pe400: hydrographic survey of the irminger sea in july 2015 for the overturning in the subpolar north atlantic program (osnap) ...
publisher SEANOE
publishDate 2019
url https://dx.doi.org/10.17882/59302
https://www.seanoe.org/data/00481/59302/
genre East Greenland
east greenland current
Greenland
North Atlantic
genre_facet East Greenland
east greenland current
Greenland
North Atlantic
op_relation https://dx.doi.org/10.4121/uuid:77b2c4fc-c253-4494-91bd-8d1ef66a014a
https://dx.doi.org/10.4121/uuid:9ae97ceb-39e4-43ec-abdb-614103285c16
https://dx.doi.org/10.1029/2023gl106501
https://dx.doi.org/10.1029/2020jc016193
https://dx.doi.org/10.1029/2018jc014730
https://dx.doi.org/10.1126/science.aau6592
https://dx.doi.org/10.1175/bams-d-16-0057.1
https://dx.doi.org/10.1002/2016gl069596
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.17882/5930210.4121/uuid:77b2c4fc-c253-4494-91bd-8d1ef66a014a10.4121/uuid:9ae97ceb-39e4-43ec-abdb-614103285c1610.1029/2023gl10650110.1029/2020jc01619310.1029/2018jc01473010.1126/science.aau659210.1175/bams-d-16-0057.110.1002/2016gl069596
_version_ 1797582024920268800