Environmental Research Letters (Jan 2018)

Tropospheric jet response to Antarctic ozone depletion: An update with Chemistry-Climate Model Initiative (CCMI) models

  • Seok-Woo Son,
  • Bo-Reum Han,
  • Chaim I Garfinkel,
  • Seo-Yeon Kim,
  • Rokjin Park,
  • N Luke Abraham,
  • Hideharu Akiyoshi,
  • Alexander T Archibald,
  • N Butchart,
  • Martyn P Chipperfield,
  • Martin Dameris,
  • Makoto Deushi,
  • Sandip S Dhomse,
  • Steven C Hardiman,
  • Patrick Jöckel,
  • Douglas Kinnison,
  • Martine Michou,
  • Olaf Morgenstern,
  • Fiona M O’Connor,
  • Luke D Oman,
  • David A Plummer,
  • Andrea Pozzer,
  • Laura E Revell,
  • Eugene Rozanov,
  • Andrea Stenke,
  • Kane Stone,
  • Simone Tilmes,
  • Yousuke Yamashita,
  • Guang Zeng

DOI
https://doi.org/10.1088/1748-9326/aabf21
Journal volume & issue
Vol. 13, no. 5
p. 054024

Abstract

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The Southern Hemisphere (SH) zonal-mean circulation change in response to Antarctic ozone depletion is re-visited by examining a set of the latest model simulations archived for the Chemistry-Climate Model Initiative (CCMI) project. All models reasonably well reproduce Antarctic ozone depletion in the late 20th century. The related SH-summer circulation changes, such as a poleward intensification of westerly jet and a poleward expansion of the Hadley cell, are also well captured. All experiments exhibit quantitatively the same multi-model mean trend, irrespective of whether the ocean is coupled or prescribed. Results are also quantitatively similar to those derived from the Coupled Model Intercomparison Project phase 5 (CMIP5) high-top model simulations in which the stratospheric ozone is mostly prescribed with monthly- and zonally-averaged values. These results suggest that the ozone-hole-induced SH-summer circulation changes are robust across the models irrespective of the specific chemistry-atmosphere-ocean coupling.

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