Rotation of floating particles in submesoscale cyclonic and anticyclonic eddies: a model study for the southeastern Baltic Sea

<p>We hypothesized that the overwhelming dominance of cyclonic spirals on satellite images of the sea surface could be caused by some differences between the rotary characteristics of submesoscale cyclonic and anticyclonic eddies. This hypothesis was tested by means of numerical experiments wi...

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Main Authors: V. Zhurbas, G. Väli, N. Kuzmina
Format: Article
Language:English
Published: Copernicus Publications 2019-12-01
Series:Ocean Science
Online Access:https://www.ocean-sci.net/15/1691/2019/os-15-1691-2019.pdf
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spelling doaj-4c7f4dfaac524e4ba34ad5e7955006f82020-11-25T02:23:34ZengCopernicus PublicationsOcean Science1812-07841812-07922019-12-01151691170510.5194/os-15-1691-2019Rotation of floating particles in submesoscale cyclonic and anticyclonic eddies: a model study for the southeastern Baltic SeaV. Zhurbas0G. Väli1N. Kuzmina2Shirshov Institute of Oceanology, Russian Academy of Sciences, 36 Nakhimovsky Prospect, 117997 Moscow, RussiaDepartment of Marine Systems, Tallinn University of Technology, Akadeemia tee 15A, 12618 Tallinn, EstoniaShirshov Institute of Oceanology, Russian Academy of Sciences, 36 Nakhimovsky Prospect, 117997 Moscow, Russia<p>We hypothesized that the overwhelming dominance of cyclonic spirals on satellite images of the sea surface could be caused by some differences between the rotary characteristics of submesoscale cyclonic and anticyclonic eddies. This hypothesis was tested by means of numerical experiments with synthetic floating Lagrangian particles embedded offline in a regional circulation model of the southeastern Baltic Sea with very high horizontal resolution (0.125 nautical mile grid). The numerical experiments showed that the cyclonic spirals can be formed from both a horizontally uniform initial distribution of floating particles and from the initially lined-up particles during an advection time of the order of 1&thinsp;d. Statistical processing of the trajectories of the synthetic floating particles allowed us to conclude that the submesoscale cyclonic eddies differ from the anticyclonic eddies in three ways favoring the formation of spirals in the tracer field: they can be characterized by (a) a considerably higher angular velocity, (b) a more pronounced differential rotation and (c) a negative helicity.</p>https://www.ocean-sci.net/15/1691/2019/os-15-1691-2019.pdf
collection DOAJ
language English
format Article
sources DOAJ
author V. Zhurbas
G. Väli
N. Kuzmina
spellingShingle V. Zhurbas
G. Väli
N. Kuzmina
Rotation of floating particles in submesoscale cyclonic and anticyclonic eddies: a model study for the southeastern Baltic Sea
Ocean Science
author_facet V. Zhurbas
G. Väli
N. Kuzmina
author_sort V. Zhurbas
title Rotation of floating particles in submesoscale cyclonic and anticyclonic eddies: a model study for the southeastern Baltic Sea
title_short Rotation of floating particles in submesoscale cyclonic and anticyclonic eddies: a model study for the southeastern Baltic Sea
title_full Rotation of floating particles in submesoscale cyclonic and anticyclonic eddies: a model study for the southeastern Baltic Sea
title_fullStr Rotation of floating particles in submesoscale cyclonic and anticyclonic eddies: a model study for the southeastern Baltic Sea
title_full_unstemmed Rotation of floating particles in submesoscale cyclonic and anticyclonic eddies: a model study for the southeastern Baltic Sea
title_sort rotation of floating particles in submesoscale cyclonic and anticyclonic eddies: a model study for the southeastern baltic sea
publisher Copernicus Publications
series Ocean Science
issn 1812-0784
1812-0792
publishDate 2019-12-01
description <p>We hypothesized that the overwhelming dominance of cyclonic spirals on satellite images of the sea surface could be caused by some differences between the rotary characteristics of submesoscale cyclonic and anticyclonic eddies. This hypothesis was tested by means of numerical experiments with synthetic floating Lagrangian particles embedded offline in a regional circulation model of the southeastern Baltic Sea with very high horizontal resolution (0.125 nautical mile grid). The numerical experiments showed that the cyclonic spirals can be formed from both a horizontally uniform initial distribution of floating particles and from the initially lined-up particles during an advection time of the order of 1&thinsp;d. Statistical processing of the trajectories of the synthetic floating particles allowed us to conclude that the submesoscale cyclonic eddies differ from the anticyclonic eddies in three ways favoring the formation of spirals in the tracer field: they can be characterized by (a) a considerably higher angular velocity, (b) a more pronounced differential rotation and (c) a negative helicity.</p>
url https://www.ocean-sci.net/15/1691/2019/os-15-1691-2019.pdf
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