Lagrangian properties of eddy fields in the northern North Atlantic as deduced from satellite-tracked buoys
One hundred and thirteen satellite-tracked buoys have been used during their first 5 months after deployment in order to calculate Lagrangian statistics of the eddy field in the northern North Atlantic between Newfoundland and the Canary basin. r.m.s. velocities are isotropic and increase from south...
Published in: | Journal of Marine Research |
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Language: | English |
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Sears Foundation of Marine Research
1987
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Online Access: | https://oceanrep.geomar.de/id/eprint/6795/ https://oceanrep.geomar.de/id/eprint/6795/1/s1.pdf https://doi.org/10.1357/002224087788401142 |
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ftoceanrep:oai:oceanrep.geomar.de:6795 2023-05-15T17:22:19+02:00 Lagrangian properties of eddy fields in the northern North Atlantic as deduced from satellite-tracked buoys Krauß, Wolfgang Böning, Claus W. 1987 text https://oceanrep.geomar.de/id/eprint/6795/ https://oceanrep.geomar.de/id/eprint/6795/1/s1.pdf https://doi.org/10.1357/002224087788401142 en eng Sears Foundation of Marine Research https://oceanrep.geomar.de/id/eprint/6795/1/s1.pdf Krauß, W. and Böning, C. W. (1987) Lagrangian properties of eddy fields in the northern North Atlantic as deduced from satellite-tracked buoys. Open Access Journal of Marine Research, 45 . pp. 259-291. DOI 10.1357/002224087788401142 <https://doi.org/10.1357/002224087788401142>. doi:10.1357/002224087788401142 cc_by_3.0 info:eu-repo/semantics/openAccess Article PeerReviewed 1987 ftoceanrep https://doi.org/10.1357/002224087788401142 2023-04-07T14:53:35Z One hundred and thirteen satellite-tracked buoys have been used during their first 5 months after deployment in order to calculate Lagrangian statistics of the eddy field in the northern North Atlantic between Newfoundland and the Canary basin. r.m.s. velocities are isotropic and increase from southeast to northwest. Lagrangian integral time scales, derived both from correlation function and from dispersion, are slightly anisotropic and decrease from the subtropics toward the North Atlantic Current. Time scale is inversely proportional to the r.m.s. velocity of the eddies. Eddy length scale is approximately constant in the North Atlantic. Dispersion is in good agreement with Taylor's hypothesis, following a t2-law during the first day after release and a linear increase with time during days 10 to 60. Eddy diffusivity increases from 30N to 50N by a factor of about 4 and is linearly dependent on the r.m.s. velocity. The energy containing frequency band of the eddies shifts toward higher frequencies in the northern part of the Atlantic. Beyond the cut-off frequency of the eddies the spectral slope follows a -2 or -3 power law. Article in Journal/Newspaper Newfoundland north atlantic current North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Journal of Marine Research 45 2 259 291 |
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Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
One hundred and thirteen satellite-tracked buoys have been used during their first 5 months after deployment in order to calculate Lagrangian statistics of the eddy field in the northern North Atlantic between Newfoundland and the Canary basin. r.m.s. velocities are isotropic and increase from southeast to northwest. Lagrangian integral time scales, derived both from correlation function and from dispersion, are slightly anisotropic and decrease from the subtropics toward the North Atlantic Current. Time scale is inversely proportional to the r.m.s. velocity of the eddies. Eddy length scale is approximately constant in the North Atlantic. Dispersion is in good agreement with Taylor's hypothesis, following a t2-law during the first day after release and a linear increase with time during days 10 to 60. Eddy diffusivity increases from 30N to 50N by a factor of about 4 and is linearly dependent on the r.m.s. velocity. The energy containing frequency band of the eddies shifts toward higher frequencies in the northern part of the Atlantic. Beyond the cut-off frequency of the eddies the spectral slope follows a -2 or -3 power law. |
format |
Article in Journal/Newspaper |
author |
Krauß, Wolfgang Böning, Claus W. |
spellingShingle |
Krauß, Wolfgang Böning, Claus W. Lagrangian properties of eddy fields in the northern North Atlantic as deduced from satellite-tracked buoys |
author_facet |
Krauß, Wolfgang Böning, Claus W. |
author_sort |
Krauß, Wolfgang |
title |
Lagrangian properties of eddy fields in the northern North Atlantic as deduced from satellite-tracked buoys |
title_short |
Lagrangian properties of eddy fields in the northern North Atlantic as deduced from satellite-tracked buoys |
title_full |
Lagrangian properties of eddy fields in the northern North Atlantic as deduced from satellite-tracked buoys |
title_fullStr |
Lagrangian properties of eddy fields in the northern North Atlantic as deduced from satellite-tracked buoys |
title_full_unstemmed |
Lagrangian properties of eddy fields in the northern North Atlantic as deduced from satellite-tracked buoys |
title_sort |
lagrangian properties of eddy fields in the northern north atlantic as deduced from satellite-tracked buoys |
publisher |
Sears Foundation of Marine Research |
publishDate |
1987 |
url |
https://oceanrep.geomar.de/id/eprint/6795/ https://oceanrep.geomar.de/id/eprint/6795/1/s1.pdf https://doi.org/10.1357/002224087788401142 |
genre |
Newfoundland north atlantic current North Atlantic |
genre_facet |
Newfoundland north atlantic current North Atlantic |
op_relation |
https://oceanrep.geomar.de/id/eprint/6795/1/s1.pdf Krauß, W. and Böning, C. W. (1987) Lagrangian properties of eddy fields in the northern North Atlantic as deduced from satellite-tracked buoys. Open Access Journal of Marine Research, 45 . pp. 259-291. DOI 10.1357/002224087788401142 <https://doi.org/10.1357/002224087788401142>. doi:10.1357/002224087788401142 |
op_rights |
cc_by_3.0 info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1357/002224087788401142 |
container_title |
Journal of Marine Research |
container_volume |
45 |
container_issue |
2 |
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259 |
op_container_end_page |
291 |
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1766108887487873024 |