Observed changes in the Southern Hemispheric circulation in May

Ivy, Diane J., Hilgenbrink, Casey, Kinnison, Doug, Plumb, R. Alan, Sheshadri, Aditi, Solomon, Susan and Thompson, David W. J. ORCID: https://orcid.org/0000-0002-5413-4376 (2017) Observed changes in the Southern Hemispheric circulation in May. Journal of Climate, 30 (2). 527–536. ISSN 0894-8755

[thumbnail of [15200442 - Journal of Climate] Observed Changes in the Southern Hemispheric Circulation in May]
PDF ([15200442 - Journal of Climate] Observed Changes in the Southern Hemispheric Circulation in May) - Published Version
Download (2MB) | Preview


Much research has focused on trends in the Southern Hemispheric circulation in austral summer (December–February) in the troposphere and stratosphere, whereas changes in other seasons have received less attention. Here the seasonality and structure of observed changes in tropospheric and stratospheric winds, temperature, and ozone over the Southern Hemisphere are examined. It is found that statistically significant trends similar to those of the Antarctic summer season are also observed since 1979 in austral fall, particularly May, and are strongest over the Pacific sector of the hemisphere. Evidence is provided for a significant shift in the position of the jet in May over the Pacific, and it is shown that the strengthening and shifting of the jet has rendered the latitudinal distribution of upper-tropospheric zonal wind more bimodal. The Antarctic ozone hole has cooled the lower stratosphere and strengthened the polar vortex. While the mechanism and timing are not fully understood, the ozone hole has been identified as a key driver of the summer season tropospheric circulation changes in several previous observational and modeling studies. It is found here that significant ozone depletion and associated polar cooling also occur in the lowermost stratosphere and tropopause region through austral fall, with spatial patterns that are coincident with the observed changes in stratospheric circulation. It is also shown that radiatively driven temperature changes associated with the observed ozone depletion in May represent a substantial portion of the observed May cooling in the lowermost stratosphere, suggesting a potential for contribution to the circulation changes.

Item Type: Article
Additional Information: Supplemental information related to this paper is available at the Journals Online website: http://dx.doi.org/10.1175/JCLI-D-16-0394.s1.
Uncontrolled Keywords: sdg 12 - responsible consumption and production ,/dk/atira/pure/sustainabledevelopmentgoals/responsible_consumption_and_production
Faculty \ School: Faculty of Science > School of Environmental Sciences
UEA Research Groups: Faculty of Science > Research Groups > Centre for Ocean and Atmospheric Sciences
Faculty of Science > Research Groups > Climatic Research Unit
Related URLs:
Depositing User: LivePure Connector
Date Deposited: 10 Jun 2022 09:30
Last Modified: 29 Jun 2023 15:30
URI: https://ueaeprints.uea.ac.uk/id/eprint/85488
DOI: 10.1175/JCLI-D-16-0394.1


Downloads per month over past year

Actions (login required)

View Item View Item