Brief communication Stratospheric winds, transport barriers and the 2011 Arctic ozone hole

Research output: Contribution to journalArticle

4 Scopus citations

Abstract

The Arctic stratosphere throughout the late winter and early spring of 2011 was characterized by an unusually severe ozone loss, resulting in what has been described as an ozone hole. The 2011 ozone loss was made possible by unusually cold temperatures throughout the Arctic stratosphere. Here we consider the issue of what constitutes suitable environmental conditions for the formation and maintenance of a polar ozone hole. Our discussion focuses on the importance of the stratospheric wind field and, in particular, the importance of a high latitude zonal jet, which serves as a meridional transport barrier both prior to ozone hole formation and during the ozone hole maintenance phase. It is argued that stratospheric conditions in the boreal winter/spring of 2011 were highly unusual inasmuch as in that year Antarctic-like Lagrangian dynamics led to the formation of a boreal ozone hole.

Original languageEnglish (US)
Pages (from-to)687-692
Number of pages6
JournalNonlinear Processes in Geophysics
Volume19
Issue number6
DOIs
StatePublished - Dec 18 2012

    Fingerprint

ASJC Scopus subject areas

  • Statistical and Nonlinear Physics
  • Geophysics
  • Geochemistry and Petrology

Cite this