Near-surface mean circulation and kinetic energy in the central North Atlantic from drifter data

An analysis of a large drifting buoy data set is presented. The objective is to obtain a self‐contained description of the properties of the near‐surface circulation (drogue depth 100 m) in the central North Atlantic Ocean, independent of hydrographic data. A necessary preanalysis step was the remov...

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Published in:Journal of Geophysical Research
Main Author: Brügge, Bernd
Format: Article in Journal/Newspaper
Language:English
Published: AGU (American Geophysical Union) 1995
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/43960/
https://oceanrep.geomar.de/id/eprint/43960/1/10.1029_95JC01501.pdf
https://doi.org/10.1029/95JC01501
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spelling ftoceanrep:oai:oceanrep.geomar.de:43960 2023-05-15T17:25:18+02:00 Near-surface mean circulation and kinetic energy in the central North Atlantic from drifter data Brügge, Bernd 1995-10-15 text https://oceanrep.geomar.de/id/eprint/43960/ https://oceanrep.geomar.de/id/eprint/43960/1/10.1029_95JC01501.pdf https://doi.org/10.1029/95JC01501 en eng AGU (American Geophysical Union) https://oceanrep.geomar.de/id/eprint/43960/1/10.1029_95JC01501.pdf Brügge, B. (1995) Near-surface mean circulation and kinetic energy in the central North Atlantic from drifter data. Open Access Journal of Geophysical Research: Oceans, 100 (C10). p. 20543. DOI 10.1029/95JC01501 <https://doi.org/10.1029/95JC01501>. doi:10.1029/95JC01501 info:eu-repo/semantics/openAccess Article PeerReviewed 1995 ftoceanrep https://doi.org/10.1029/95JC01501 2023-04-07T15:40:50Z An analysis of a large drifting buoy data set is presented. The objective is to obtain a self‐contained description of the properties of the near‐surface circulation (drogue depth 100 m) in the central North Atlantic Ocean, independent of hydrographic data. A necessary preanalysis step was the removal of all data from undrogued buoys from the data set. The physical parameters of the circulation were deduced by averaging the remaining data in 2°×3° boxes. The minimum amount of data which is necessary to get statistically stable results was determined by an empirical quality criterion. All important mean currents in the investigation area are reproduced by the near‐surface mean velocity field. A separation of the mean velocity field into a nondivergent and an irrational part shows that the flow field is almost nondivergent. The distribution of eddy kinetic energy is concentrated along the mean currents and provides the largest part of the total kinetic energy, but there are regional variations. Energy from inertial movements dominates the high‐frequency part of the kinetic energy. Its distribution is very patchy. The analysis of the Reynolds stress terms shows an energy transfer from the eddy field to the mean circulation in the vicinity of the North Atlantic Current. Article in Journal/Newspaper north atlantic current North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Journal of Geophysical Research 100 C10 20543
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
description An analysis of a large drifting buoy data set is presented. The objective is to obtain a self‐contained description of the properties of the near‐surface circulation (drogue depth 100 m) in the central North Atlantic Ocean, independent of hydrographic data. A necessary preanalysis step was the removal of all data from undrogued buoys from the data set. The physical parameters of the circulation were deduced by averaging the remaining data in 2°×3° boxes. The minimum amount of data which is necessary to get statistically stable results was determined by an empirical quality criterion. All important mean currents in the investigation area are reproduced by the near‐surface mean velocity field. A separation of the mean velocity field into a nondivergent and an irrational part shows that the flow field is almost nondivergent. The distribution of eddy kinetic energy is concentrated along the mean currents and provides the largest part of the total kinetic energy, but there are regional variations. Energy from inertial movements dominates the high‐frequency part of the kinetic energy. Its distribution is very patchy. The analysis of the Reynolds stress terms shows an energy transfer from the eddy field to the mean circulation in the vicinity of the North Atlantic Current.
format Article in Journal/Newspaper
author Brügge, Bernd
spellingShingle Brügge, Bernd
Near-surface mean circulation and kinetic energy in the central North Atlantic from drifter data
author_facet Brügge, Bernd
author_sort Brügge, Bernd
title Near-surface mean circulation and kinetic energy in the central North Atlantic from drifter data
title_short Near-surface mean circulation and kinetic energy in the central North Atlantic from drifter data
title_full Near-surface mean circulation and kinetic energy in the central North Atlantic from drifter data
title_fullStr Near-surface mean circulation and kinetic energy in the central North Atlantic from drifter data
title_full_unstemmed Near-surface mean circulation and kinetic energy in the central North Atlantic from drifter data
title_sort near-surface mean circulation and kinetic energy in the central north atlantic from drifter data
publisher AGU (American Geophysical Union)
publishDate 1995
url https://oceanrep.geomar.de/id/eprint/43960/
https://oceanrep.geomar.de/id/eprint/43960/1/10.1029_95JC01501.pdf
https://doi.org/10.1029/95JC01501
genre north atlantic current
North Atlantic
genre_facet north atlantic current
North Atlantic
op_relation https://oceanrep.geomar.de/id/eprint/43960/1/10.1029_95JC01501.pdf
Brügge, B. (1995) Near-surface mean circulation and kinetic energy in the central North Atlantic from drifter data. Open Access Journal of Geophysical Research: Oceans, 100 (C10). p. 20543. DOI 10.1029/95JC01501 <https://doi.org/10.1029/95JC01501>.
doi:10.1029/95JC01501
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1029/95JC01501
container_title Journal of Geophysical Research
container_volume 100
container_issue C10
container_start_page 20543
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