Single super-vortex as a proxy for ocean surface flow fields

<p>Empirical flow field data evaluation in a well-studied ocean region along the US west coast revealed a surprisingly strong relationship between the surface integrals of kinetic energy and enstrophy (squared vorticity). This relationship defines a single isolated Gaussian super-vortex, whose...

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Main Authors: I. M. Jánosi, M. Vincze, G. Tóth, J. A. C. Gallas
Format: Article
Language:English
Published: Copernicus Publications 2019-07-01
Series:Ocean Science
Online Access:https://www.ocean-sci.net/15/941/2019/os-15-941-2019.pdf
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spelling doaj-71776fdd4f9b41d7828829dd094197b82020-11-25T01:55:04ZengCopernicus PublicationsOcean Science1812-07841812-07922019-07-011594194910.5194/os-15-941-2019Single super-vortex as a proxy for ocean surface flow fieldsI. M. Jánosi0I. M. Jánosi1I. M. Jánosi2M. Vincze3M. Vincze4G. Tóth5J. A. C. Gallas6J. A. C. Gallas7J. A. C. Gallas8Department of Physics of Complex Systems, Eötvös Loránd University, Pázmány Péter s. 1/A, 1117 Budapest, HungaryMax Planck Institute for the Physics of Complex Systems, Nöthnitzer Str. 38, 01187 Dresden, Germanyvon Kármán Laboratory for Environmental Flows, Eötvös Loránd University, Pázmány Péter s. 1/A, 1117 Budapest, Hungaryvon Kármán Laboratory for Environmental Flows, Eötvös Loránd University, Pázmány Péter s. 1/A, 1117 Budapest, HungaryMTA-ELTE Theoretical Physics Research Group, Pázmány Péter s. 1/A, 1117 Budapest, HungaryDepartment of Physics of Complex Systems, Eötvös Loránd University, Pázmány Péter s. 1/A, 1117 Budapest, HungaryMax Planck Institute for the Physics of Complex Systems, Nöthnitzer Str. 38, 01187 Dresden, GermanyComplexity Sciences Center, 9225 Collins Avenue Suite 1208, Surfside, FL 33154, USAInstituto de Altos Estudos da Paraíba, Rua Silvino Lopes 419-2502, 58039-190 João Pessoa, Brazil<p>Empirical flow field data evaluation in a well-studied ocean region along the US west coast revealed a surprisingly strong relationship between the surface integrals of kinetic energy and enstrophy (squared vorticity). This relationship defines a single isolated Gaussian super-vortex, whose fitted size parameter is related to the mean eddy size, and the square of the fitted height parameter is proportional to the sum of the square of all individual eddy amplitudes obtained by standard vortex census. This finding allows very effective coarse-grained eddy statistics with minimal computational efforts. As an illustrative example, the westward drift velocity of eddies is determined from a simple cross-correlation analysis of kinetic energy integrals.</p>https://www.ocean-sci.net/15/941/2019/os-15-941-2019.pdf
collection DOAJ
language English
format Article
sources DOAJ
author I. M. Jánosi
I. M. Jánosi
I. M. Jánosi
M. Vincze
M. Vincze
G. Tóth
J. A. C. Gallas
J. A. C. Gallas
J. A. C. Gallas
spellingShingle I. M. Jánosi
I. M. Jánosi
I. M. Jánosi
M. Vincze
M. Vincze
G. Tóth
J. A. C. Gallas
J. A. C. Gallas
J. A. C. Gallas
Single super-vortex as a proxy for ocean surface flow fields
Ocean Science
author_facet I. M. Jánosi
I. M. Jánosi
I. M. Jánosi
M. Vincze
M. Vincze
G. Tóth
J. A. C. Gallas
J. A. C. Gallas
J. A. C. Gallas
author_sort I. M. Jánosi
title Single super-vortex as a proxy for ocean surface flow fields
title_short Single super-vortex as a proxy for ocean surface flow fields
title_full Single super-vortex as a proxy for ocean surface flow fields
title_fullStr Single super-vortex as a proxy for ocean surface flow fields
title_full_unstemmed Single super-vortex as a proxy for ocean surface flow fields
title_sort single super-vortex as a proxy for ocean surface flow fields
publisher Copernicus Publications
series Ocean Science
issn 1812-0784
1812-0792
publishDate 2019-07-01
description <p>Empirical flow field data evaluation in a well-studied ocean region along the US west coast revealed a surprisingly strong relationship between the surface integrals of kinetic energy and enstrophy (squared vorticity). This relationship defines a single isolated Gaussian super-vortex, whose fitted size parameter is related to the mean eddy size, and the square of the fitted height parameter is proportional to the sum of the square of all individual eddy amplitudes obtained by standard vortex census. This finding allows very effective coarse-grained eddy statistics with minimal computational efforts. As an illustrative example, the westward drift velocity of eddies is determined from a simple cross-correlation analysis of kinetic energy integrals.</p>
url https://www.ocean-sci.net/15/941/2019/os-15-941-2019.pdf
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