Insights into the three-dimensional lagrangian geometry of the Antarctic polar vortex

In this paper we study the three-dimensional (3-D) Lagrangian structures in the stratospheric polar vortex (SPV) above Antarctica. We analyse and visualize these structures using Lagrangian descriptor function M. The procedure for calculation with reanalysis data is explained. Benchmarks are compute...

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Published in:Nonlinear Processes in Geophysics
Main Authors: Curbelo, Jezabel, García-Garrido, Víctor José, Roberto Mechoso, Carlos, Mancho, Ana Maria, Wiggins, Stephen, Niang, Coumba
Other Authors: Ministerio de Economía y Competitividad (España), Consejo Superior de Investigaciones Científicas https://ror.org/02gfc7t72
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:http://hdl.handle.net/10261/255750
https://doi.org/10.5194/npg-24-379-2017
https://doi.org/10.13039/501100003329
https://api.elsevier.com/content/abstract/scopus_id/85025822746
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author Curbelo, Jezabel
García-Garrido, Víctor José
Roberto Mechoso, Carlos
Mancho, Ana Maria
Wiggins, Stephen
Niang, Coumba
author2 Ministerio de Economía y Competitividad (España)
Consejo Superior de Investigaciones Científicas https://ror.org/02gfc7t72
author_facet Curbelo, Jezabel
García-Garrido, Víctor José
Roberto Mechoso, Carlos
Mancho, Ana Maria
Wiggins, Stephen
Niang, Coumba
author_sort Curbelo, Jezabel
collection Digital.CSIC (Spanish National Research Council)
container_issue 3
container_start_page 379
container_title Nonlinear Processes in Geophysics
container_volume 24
description In this paper we study the three-dimensional (3-D) Lagrangian structures in the stratospheric polar vortex (SPV) above Antarctica. We analyse and visualize these structures using Lagrangian descriptor function M. The procedure for calculation with reanalysis data is explained. Benchmarks are computed and analysed that allow us to compare 2-D and 3-D aspects of Lagrangian transport. Dynamical systems concepts appropriate to 3-D, such as normally hyperbolic invariant curves, are discussed and applied. In order to illustrate our approach we select an interval of time in which the SPV is relatively undisturbed (August 1979) and an interval of rapid SPV changes (October 1979). Our results provide new insights into the Lagrangian structure of the vertical extension of the stratospheric polar vortex and its evolution. Our results also show complex Lagrangian patterns indicative of strong mixing processes in the upper troposphere and lower stratosphere. Finally, during the transition to summer in the late spring, we illustrate the vertical structure of two counterrotating vortices, one the polar and the other an emerging one, and the invariant separatrix that divides them. Jezabel Curbelo, Víctor José García-Garrido and Ana Maria Mancho are supported by MINECO grant MTM2014-56392-R. Coumba Niang acknowledges Fundacion Mujeres por Africa and ICMAT Severo Ochoa project SEV-2011- 0087 for financial support. Ana Maria Mancho and Coumba Niang are supported by CSIC grant COOPB20265. The research of Stephen Wiggins is supported by ONR grant no. N00014-01-1- 0769. Carlos Roberto Mechoso was supported by U.S. NSF grant AGS-1245069. We also acknowledge support from ONR grant no. N00014-16-1-2492. Thanks are owed to CESGA and ICMAT for computing facilities. Peer reviewed
format Article in Journal/Newspaper
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
geographic Antarctic
Garrido
The Antarctic
geographic_facet Antarctic
Garrido
The Antarctic
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institution Open Polar
language English
long_lat ENVELOPE(-57.067,-57.067,-63.500,-63.500)
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op_doi https://doi.org/10.5194/npg-24-379-201710.13039/501100003329
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info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/56392
Nonlinear Processes in Geophysics
Publisher's version

10235809
http://hdl.handle.net/10261/255750
http://dx.doi.org/10.13039/501100003329
https://api.elsevier.com/content/abstract/scopus_id/85025822746
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spelling ftcsic:oai:digital.csic.es:10261/255750 2025-01-16T19:42:45+00:00 Insights into the three-dimensional lagrangian geometry of the Antarctic polar vortex Curbelo, Jezabel García-Garrido, Víctor José Roberto Mechoso, Carlos Mancho, Ana Maria Wiggins, Stephen Niang, Coumba Ministerio de Economía y Competitividad (España) Consejo Superior de Investigaciones Científicas https://ror.org/02gfc7t72 2017-07-25 http://hdl.handle.net/10261/255750 https://doi.org/10.5194/npg-24-379-2017 https://doi.org/10.13039/501100003329 https://api.elsevier.com/content/abstract/scopus_id/85025822746 en eng #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/56392 Nonlinear Processes in Geophysics Publisher's version Sí 10235809 http://hdl.handle.net/10261/255750 http://dx.doi.org/10.13039/501100003329 https://api.elsevier.com/content/abstract/scopus_id/85025822746 open artículo http://purl.org/coar/resource_type/c_6501 2017 ftcsic https://doi.org/10.5194/npg-24-379-201710.13039/501100003329 2024-11-05T15:44:17Z In this paper we study the three-dimensional (3-D) Lagrangian structures in the stratospheric polar vortex (SPV) above Antarctica. We analyse and visualize these structures using Lagrangian descriptor function M. The procedure for calculation with reanalysis data is explained. Benchmarks are computed and analysed that allow us to compare 2-D and 3-D aspects of Lagrangian transport. Dynamical systems concepts appropriate to 3-D, such as normally hyperbolic invariant curves, are discussed and applied. In order to illustrate our approach we select an interval of time in which the SPV is relatively undisturbed (August 1979) and an interval of rapid SPV changes (October 1979). Our results provide new insights into the Lagrangian structure of the vertical extension of the stratospheric polar vortex and its evolution. Our results also show complex Lagrangian patterns indicative of strong mixing processes in the upper troposphere and lower stratosphere. Finally, during the transition to summer in the late spring, we illustrate the vertical structure of two counterrotating vortices, one the polar and the other an emerging one, and the invariant separatrix that divides them. Jezabel Curbelo, Víctor José García-Garrido and Ana Maria Mancho are supported by MINECO grant MTM2014-56392-R. Coumba Niang acknowledges Fundacion Mujeres por Africa and ICMAT Severo Ochoa project SEV-2011- 0087 for financial support. Ana Maria Mancho and Coumba Niang are supported by CSIC grant COOPB20265. The research of Stephen Wiggins is supported by ONR grant no. N00014-01-1- 0769. Carlos Roberto Mechoso was supported by U.S. NSF grant AGS-1245069. We also acknowledge support from ONR grant no. N00014-16-1-2492. Thanks are owed to CESGA and ICMAT for computing facilities. Peer reviewed Article in Journal/Newspaper Antarc* Antarctic Antarctica Digital.CSIC (Spanish National Research Council) Antarctic Garrido ENVELOPE(-57.067,-57.067,-63.500,-63.500) The Antarctic Nonlinear Processes in Geophysics 24 3 379 392
spellingShingle Curbelo, Jezabel
García-Garrido, Víctor José
Roberto Mechoso, Carlos
Mancho, Ana Maria
Wiggins, Stephen
Niang, Coumba
Insights into the three-dimensional lagrangian geometry of the Antarctic polar vortex
title Insights into the three-dimensional lagrangian geometry of the Antarctic polar vortex
title_full Insights into the three-dimensional lagrangian geometry of the Antarctic polar vortex
title_fullStr Insights into the three-dimensional lagrangian geometry of the Antarctic polar vortex
title_full_unstemmed Insights into the three-dimensional lagrangian geometry of the Antarctic polar vortex
title_short Insights into the three-dimensional lagrangian geometry of the Antarctic polar vortex
title_sort insights into the three-dimensional lagrangian geometry of the antarctic polar vortex
url http://hdl.handle.net/10261/255750
https://doi.org/10.5194/npg-24-379-2017
https://doi.org/10.13039/501100003329
https://api.elsevier.com/content/abstract/scopus_id/85025822746