Nonlinear features of equatorial baroclinic Rossby waves detected in Topex altimeter observations

Using a recently proposed technique for statistical analysis of non-gridded satellite altimeter data, regime of long equatorially-trapped baroclinic Rossby waves is studied. One-dimensional spatial and spatiotemporal autocorrelation functions of sea surface height (SSH) variations yi...

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Main Authors: R. E. Glazman, A. Fabrikant, A. M. Greysukh
Format: Article
Language:English
Published: Copernicus Publications 1996-01-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/3/115/1996/npg-3-115-1996.pdf
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author R. E. Glazman
A. Fabrikant
A. Fabrikant
A. M. Greysukh
author_facet R. E. Glazman
A. Fabrikant
A. Fabrikant
A. M. Greysukh
author_sort R. E. Glazman
collection DOAJ
description Using a recently proposed technique for statistical analysis of non-gridded satellite altimeter data, regime of long equatorially-trapped baroclinic Rossby waves is studied. One-dimensional spatial and spatiotemporal autocorrelation functions of sea surface height (SSH) variations yield a broad spectrum of baroclinic Rossby waves and permit determination of their propagation speed. The 1-d wavenumber spectrum of zonal variations is given by a power-law k<em><sup>-2</sup></em> on scales from about 10<sup><em>3</em> </sup> km to 10<sup>4</sup> km. We demonstrate that the observed wave regime exhibits features of soliton turbulence developing in the long baroclinic Rossby waves. However, being limited to second statistical moments, the present analysis does not allow us to rule out a possibility of weak wave turbulence.
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spelling doaj.art-4b551b3ae61a492fb472a50a82d56a152022-12-21T19:31:54ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79461996-01-0132115126Nonlinear features of equatorial baroclinic Rossby waves detected in Topex altimeter observationsR. E. GlazmanA. FabrikantA. FabrikantA. M. GreysukhUsing a recently proposed technique for statistical analysis of non-gridded satellite altimeter data, regime of long equatorially-trapped baroclinic Rossby waves is studied. One-dimensional spatial and spatiotemporal autocorrelation functions of sea surface height (SSH) variations yield a broad spectrum of baroclinic Rossby waves and permit determination of their propagation speed. The 1-d wavenumber spectrum of zonal variations is given by a power-law k<em><sup>-2</sup></em> on scales from about 10<sup><em>3</em> </sup> km to 10<sup>4</sup> km. We demonstrate that the observed wave regime exhibits features of soliton turbulence developing in the long baroclinic Rossby waves. However, being limited to second statistical moments, the present analysis does not allow us to rule out a possibility of weak wave turbulence.http://www.nonlin-processes-geophys.net/3/115/1996/npg-3-115-1996.pdf
spellingShingle R. E. Glazman
A. Fabrikant
A. Fabrikant
A. M. Greysukh
Nonlinear features of equatorial baroclinic Rossby waves detected in Topex altimeter observations
Nonlinear Processes in Geophysics
title Nonlinear features of equatorial baroclinic Rossby waves detected in Topex altimeter observations
title_full Nonlinear features of equatorial baroclinic Rossby waves detected in Topex altimeter observations
title_fullStr Nonlinear features of equatorial baroclinic Rossby waves detected in Topex altimeter observations
title_full_unstemmed Nonlinear features of equatorial baroclinic Rossby waves detected in Topex altimeter observations
title_short Nonlinear features of equatorial baroclinic Rossby waves detected in Topex altimeter observations
title_sort nonlinear features of equatorial baroclinic rossby waves detected in topex altimeter observations
url http://www.nonlin-processes-geophys.net/3/115/1996/npg-3-115-1996.pdf
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