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 comput...

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Published in:Nonlinear Processes in Geophysics
Main Authors: J. Curbelo, V. J. García-Garrido, C. R. Mechoso, A. M. Mancho, S. Wiggins, C. Niang
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2017
Subjects:
Online Access:https://doi.org/10.5194/npg-24-379-2017
https://doaj.org/article/2db016a6d90e4930a887a543210b9022
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author J. Curbelo
V. J. García-Garrido
C. R. Mechoso
A. M. Mancho
S. Wiggins
C. Niang
author_facet J. Curbelo
V. J. García-Garrido
C. R. Mechoso
A. M. Mancho
S. Wiggins
C. Niang
author_sort J. Curbelo
collection Directory of Open Access Journals: DOAJ Articles
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.
format Article in Journal/Newspaper
genre Antarc*
Antarctic
Antarctica
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Antarctica
geographic Antarctic
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spelling ftdoajarticles:oai:doaj.org/article:2db016a6d90e4930a887a543210b9022 2025-01-16T19:19:54+00:00 Insights into the three-dimensional Lagrangian geometry of the Antarctic polar vortex J. Curbelo V. J. García-Garrido C. R. Mechoso A. M. Mancho S. Wiggins C. Niang 2017-07-01T00:00:00Z https://doi.org/10.5194/npg-24-379-2017 https://doaj.org/article/2db016a6d90e4930a887a543210b9022 EN eng Copernicus Publications https://www.nonlin-processes-geophys.net/24/379/2017/npg-24-379-2017.pdf https://doaj.org/toc/1023-5809 https://doaj.org/toc/1607-7946 doi:10.5194/npg-24-379-2017 1023-5809 1607-7946 https://doaj.org/article/2db016a6d90e4930a887a543210b9022 Nonlinear Processes in Geophysics, Vol 24, Pp 379-392 (2017) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 2017 ftdoajarticles https://doi.org/10.5194/npg-24-379-2017 2022-12-31T01:11:36Z 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. Article in Journal/Newspaper Antarc* Antarctic Antarctica Directory of Open Access Journals: DOAJ Articles Antarctic The Antarctic Nonlinear Processes in Geophysics 24 3 379 392
spellingShingle Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
J. Curbelo
V. J. García-Garrido
C. R. Mechoso
A. M. Mancho
S. Wiggins
C. Niang
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
topic Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
topic_facet Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
url https://doi.org/10.5194/npg-24-379-2017
https://doaj.org/article/2db016a6d90e4930a887a543210b9022