Journal cover Journal topic
Nonlinear Processes in Geophysics An interactive open-access journal of the European Geosciences Union

Journal metrics

  • IF value: 1.329 IF 1.329
  • IF 5-year<br/> value: 1.394 IF 5-year
    1.394
  • CiteScore<br/> value: 1.27 CiteScore
    1.27
  • SNIP value: 0.903 SNIP 0.903
  • SJR value: 0.709 SJR 0.709
  • IPP value: 1.455 IPP 1.455
  • h5-index value: 20 h5-index 20
https://doi.org/10.5194/npg-2017-8
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
16 Feb 2017
Review status
A revision of this discussion paper was accepted for the journal Nonlinear Processes in Geophysics (NPG) and is expected to appear here in due course.
Insights on the three-dimensional Lagrangian geometry of the Antarctic Polar Vortex
Jezabel Curbelo1,2, Victor J. García-Garrido1, Carlos R. Mechoso3, Ana M. Mancho1, Stephen Wiggins4, and Coumba Niang1,5 1Instituto de Ciencias Matemáticas, CSIC-UAM-UC3M-UCM. C/ Nicolás Cabrera 15, Campus de Cantoblanco UAM, 28049 Madrid, Spain
2Departamento de Matemáticas, Facultad de Ciencias, Universidad Autonóma de Madrid, 28049 Madrid, Spain
3Department of Atmospheric and Oceanic Sciences, University of California at Los Angeles, Los Angeles, California, USA
4School of Mathematics, University of Bristol. Bristol BS8 1TW, UK
5Laboratoire de Physique de l’Atmosphere et de l’Ocean Simeon Fongang, Ecole Superieure Polytechnique, Universite Cheikh Anta Diop, 5085, Dakar-Fann, Senegal
Abstract. The present paper introduces an algorithm for the visualization, analysis and verification of transport and mixing processes in three-dimensional atmospheric flows. This algorithm is based on the methodology of Lagrangian descriptors (LDs), a technique from Dynamical Systems Theory. The algorithm is applied to reanalysis data in order to illustrate the evolution of the flow above Antarctica during a period of rapid changes in the southern spring of 1979. The evolution of Lagrangian coherent structures is discussed and connections with the stratosphere is examined. The results suggest that the cyclonic stratospheric polar vortex during late winter appears to extend down to the troposphere. The results are also indicative of features related to invariante manifolds that can act as deep vertical barriers to transport between vortices.

Citation: Curbelo, J., García-Garrido, V. J., Mechoso, C. R., Mancho, A. M., Wiggins, S., and Niang, C.: Insights on the three-dimensional Lagrangian geometry of the Antarctic Polar Vortex, Nonlin. Processes Geophys. Discuss., https://doi.org/10.5194/npg-2017-8, in review, 2017.
Jezabel Curbelo et al.
Interactive discussionStatus: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version      Supplement - Supplement
 
RC1: 'Review', Anonymous Referee #1, 07 Mar 2017 Printer-friendly Version 
AC1: 'Response to anonymous referee #1', Ana M. Mancho, 08 Jun 2017 Printer-friendly Version Supplement 
 
RC2: 'Referee report', Anonymous Referee #2, 15 Mar 2017 Printer-friendly Version 
AC2: 'Response to anonymous referee #2', Ana M. Mancho, 08 Jun 2017 Printer-friendly Version Supplement 
Jezabel Curbelo et al.
Jezabel Curbelo et al.

Viewed

Total article views: 339 (including HTML, PDF, and XML)

HTML PDF XML Total Supplement BibTeX EndNote
259 45 35 339 42 3 33

Views and downloads (calculated since 16 Feb 2017)

Cumulative views and downloads (calculated since 16 Feb 2017)

Viewed (geographical distribution)

Total article views: 339 (including HTML, PDF, and XML)

Thereof 338 with geography defined and 1 with unknown origin.

Country # Views %
  • 1

Saved

Discussed

Latest update: 27 Jun 2017
Publications Copernicus
Download
Share