Lagrangian methods for observation of intrathermocline eddies in ocean
Intrathermocline anticyclonic eddies (lenses) of Mediterranean origin are regularly observed in the Eastern part of the Atlantic Ocean. These eddies are identified both from satellites as altimetry and seasurface temperature (SST) changes and according to data of neutral buoyancy floats (NBF) placed...
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Published in | Oceanology (Washington. 1965) Vol. 54; no. 6; pp. 688 - 694 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
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Moscow
Pleiades Publishing
01.11.2014
Springer Nature B.V |
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Abstract | Intrathermocline anticyclonic eddies (lenses) of Mediterranean origin are regularly observed in the Eastern part of the Atlantic Ocean. These eddies are identified both from satellites as altimetry and seasurface temperature (SST) changes and according to data of neutral buoyancy floats (NBF) placed in the body of a lens. In this paper, in the framework of a three-layer quasi-geostrophic model, using the contour dynamics method, we consider some theoretical aspects of lens movement observations made by acoustic NBF and freely drifting buoys of the Argo project. Direct experimental observation data on the lenses’ drift in the North Atlantic qualitatively confirmed the results of our numerical experiments. In particular, it is shown that the spin of the lens has an advective influence on the behavior of NBF at distances of several lens radii. |
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AbstractList | Intrathermocline anticyclonic eddies (lenses) of Mediterranean origin are regularly observed in the Eastern part of the Atlantic Ocean. These eddies are identified both from satellites as altimetry and seasurface temperature (SST) changes and according to data of neutral buoyancy floats (NBF) placed in the body of a lens. In this paper, in the framework of a three-layer quasi-geostrophic model, using the contour dynamics method, we consider some theoretical aspects of lens movement observations made by acoustic NBF and freely drifting buoys of the Argo project. Direct experimental observation data on the lenses' drift in the North Atlantic qualitatively confirmed the results of our numerical experiments. In particular, it is shown that the spin of the lens has an advective influence on the behavior of NBF at distances of several lens radii.[PUBLICATION ABSTRACT] Intrathermocline anticyclonic eddies (lenses) of Mediterranean origin are regularly observed in the Eastern part of the Atlantic Ocean. These eddies are identified both from satellites as altimetry and seasurface temperature (SST) changes and according to data of neutral buoyancy floats (NBF) placed in the body of a lens. In this paper, in the framework of a three-layer quasi-geostrophic model, using the contour dynamics method, we consider some theoretical aspects of lens movement observations made by acoustic NBF and freely drifting buoys of the Argo project. Direct experimental observation data on the lenses’ drift in the North Atlantic qualitatively confirmed the results of our numerical experiments. In particular, it is shown that the spin of the lens has an advective influence on the behavior of NBF at distances of several lens radii. |
Author | Vagina, I. M. Kozhelupova, N. G. Sokolovskiy, M. A. Filyushkin, B. N. |
Author_xml | – sequence: 1 givenname: B. N. surname: Filyushkin fullname: Filyushkin, B. N. email: borfil@ioran.ru organization: Shirshov Institute of Oceanology, Russian Academy of Sciences – sequence: 2 givenname: M. A. surname: Sokolovskiy fullname: Sokolovskiy, M. A. organization: Water Problems Institute, Russian Academy of Sciences – sequence: 3 givenname: N. G. surname: Kozhelupova fullname: Kozhelupova, N. G. organization: Shirshov Institute of Oceanology, Russian Academy of Sciences – sequence: 4 givenname: I. M. surname: Vagina fullname: Vagina, I. M. organization: Moscow State University |
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CitedBy_id | crossref_primary_10_1088_1755_1315_459_5_052100 crossref_primary_10_1080_03091929_2016_1164148 crossref_primary_10_1103_PhysRevE_92_053021 crossref_primary_10_1007_s00343_020_9313_4 |
Cites_doi | 10.1029/2009JC005646 10.1134/S1028334X1010020X 10.1007/s10236-013-0628-y 10.5194/npg-20-437-2013 10.1175/1520-0485(1989)019<0354:TYITLO>2.0.CO;2 10.1134/S1028334X11120269 10.1175/1520-0485(1989)019<0371:TTMWSF>2.0.CO;2 10.1357/002224011798765231 10.1029/90JC02740 10.1357/002224011798765204 10.5194/os-8-931-2012 10.1134/S1028334X11070063 |
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SubjectTerms | Altimetry Earth and Environmental Science Earth Sciences Eddies Floats Marine Marine Physics Ocean circulation Ocean currents Oceanography |
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Title | Lagrangian methods for observation of intrathermocline eddies in ocean |
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