Mean circulation and EKE distribution in the Labrador Sea Water level of the subpolar North Atlantic ...

A long-term mean flow field for the subpolar North Atlantic region with a horizontal resolution of approximately 25km is created by gridding Argo-derived velocity vectors using two different topography-following interpolation schemes. The 10-day float displacements in the typical drift depths of 100...

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Main Authors: Fischer, Jürgen, Karstensen, Johannes, Oltmanns, Marilena, Schmidtko, Sunke
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2018
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.894949
https://doi.pangaea.de/10.1594/PANGAEA.894949
id ftdatacite:10.1594/pangaea.894949
record_format openpolar
spelling ftdatacite:10.1594/pangaea.894949 2024-03-31T07:53:47+00:00 Mean circulation and EKE distribution in the Labrador Sea Water level of the subpolar North Atlantic ... Fischer, Jürgen Karstensen, Johannes Oltmanns, Marilena Schmidtko, Sunke 2018 application/zip https://dx.doi.org/10.1594/pangaea.894949 https://doi.pangaea.de/10.1594/PANGAEA.894949 en eng PANGAEA https://dx.doi.org/10.5194/os-14-1167-2018 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Optimizing and Enhancing the Integrated Atlantic Ocean Observing System AtlantOS Regional Atlantic Circulation and global Change RACE Supplementary Publication Series of Datasets article Collection 2018 ftdatacite https://doi.org/10.1594/pangaea.89494910.5194/os-14-1167-2018 2024-03-04T14:19:23Z A long-term mean flow field for the subpolar North Atlantic region with a horizontal resolution of approximately 25km is created by gridding Argo-derived velocity vectors using two different topography-following interpolation schemes. The 10-day float displacements in the typical drift depths of 1000 to 1500m represent the flow in the Labrador Sea Water density range. Both mapping algorithms separate the flow field into potential vorticity (PV) conserving, i.e., topography-following contribution and a deviating part, which we define as the eddy contribution. To verify the significance of the separation, we compare the mean flow and the eddy kinetic energy (EKE), derived from both mapping algorithms, with those obtained from multiyear mooring observations. ... : Supplement to: Fischer, Jürgen; Karstensen, Johannes; Oltmanns, Marilena; Schmidtko, Sunke (2018): Mean circulation and EKE distribution in the Labrador Sea Water level of the subpolar North Atlantic. Ocean Science, 14(5), 1167-1183 ... Article in Journal/Newspaper Labrador Sea 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 English
topic Optimizing and Enhancing the Integrated Atlantic Ocean Observing System AtlantOS
Regional Atlantic Circulation and global Change RACE
spellingShingle Optimizing and Enhancing the Integrated Atlantic Ocean Observing System AtlantOS
Regional Atlantic Circulation and global Change RACE
Fischer, Jürgen
Karstensen, Johannes
Oltmanns, Marilena
Schmidtko, Sunke
Mean circulation and EKE distribution in the Labrador Sea Water level of the subpolar North Atlantic ...
topic_facet Optimizing and Enhancing the Integrated Atlantic Ocean Observing System AtlantOS
Regional Atlantic Circulation and global Change RACE
description A long-term mean flow field for the subpolar North Atlantic region with a horizontal resolution of approximately 25km is created by gridding Argo-derived velocity vectors using two different topography-following interpolation schemes. The 10-day float displacements in the typical drift depths of 1000 to 1500m represent the flow in the Labrador Sea Water density range. Both mapping algorithms separate the flow field into potential vorticity (PV) conserving, i.e., topography-following contribution and a deviating part, which we define as the eddy contribution. To verify the significance of the separation, we compare the mean flow and the eddy kinetic energy (EKE), derived from both mapping algorithms, with those obtained from multiyear mooring observations. ... : Supplement to: Fischer, Jürgen; Karstensen, Johannes; Oltmanns, Marilena; Schmidtko, Sunke (2018): Mean circulation and EKE distribution in the Labrador Sea Water level of the subpolar North Atlantic. Ocean Science, 14(5), 1167-1183 ...
format Article in Journal/Newspaper
author Fischer, Jürgen
Karstensen, Johannes
Oltmanns, Marilena
Schmidtko, Sunke
author_facet Fischer, Jürgen
Karstensen, Johannes
Oltmanns, Marilena
Schmidtko, Sunke
author_sort Fischer, Jürgen
title Mean circulation and EKE distribution in the Labrador Sea Water level of the subpolar North Atlantic ...
title_short Mean circulation and EKE distribution in the Labrador Sea Water level of the subpolar North Atlantic ...
title_full Mean circulation and EKE distribution in the Labrador Sea Water level of the subpolar North Atlantic ...
title_fullStr Mean circulation and EKE distribution in the Labrador Sea Water level of the subpolar North Atlantic ...
title_full_unstemmed Mean circulation and EKE distribution in the Labrador Sea Water level of the subpolar North Atlantic ...
title_sort mean circulation and eke distribution in the labrador sea water level of the subpolar north atlantic ...
publisher PANGAEA
publishDate 2018
url https://dx.doi.org/10.1594/pangaea.894949
https://doi.pangaea.de/10.1594/PANGAEA.894949
genre Labrador Sea
North Atlantic
genre_facet Labrador Sea
North Atlantic
op_relation https://dx.doi.org/10.5194/os-14-1167-2018
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/10.1594/pangaea.89494910.5194/os-14-1167-2018
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