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 inOceanology (Washington. 1965) Vol. 54; no. 6; pp. 688 - 694
Main Authors Filyushkin, B. N., Sokolovskiy, M. A., Kozhelupova, N. G., Vagina, I. M.
Format Journal Article
LanguageEnglish
Published 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.
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.
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CitedBy_id crossref_primary_10_1088_1755_1315_459_5_052100
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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
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10.1029/90JC02740
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10.1134/S1028334X11070063
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Snippet Intrathermocline anticyclonic eddies (lenses) of Mediterranean origin are regularly observed in the Eastern part of the Atlantic Ocean. These eddies are...
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springer
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StartPage 688
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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