Australian rainfall and surface temperature variations associated with the Southern Hemisphere annular mode

Hendon, Harry H., Thompson, David W. J. ORCID: https://orcid.org/0000-0002-5413-4376 and Wheeler, Matthew C. (2007) Australian rainfall and surface temperature variations associated with the Southern Hemisphere annular mode. Journal of Climate, 20 (11). 2452–2467. ISSN 0894-8755

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Abstract

Daily variations in Australian rainfall and surface temperature associated with the Southern Hemisphere annular mode (SAM) are documented using observations for the period 1979–2005. The high index polarity of the SAM is characterized by a poleward contraction of the midlatitude westerlies. During winter, the high index polarity of the SAM is associated with decreased daily rainfall over southeast and southwest Australia, but during summer it is associated with increased daily rainfall on the southern east coast of Australia and decreased rainfall in western Tasmania. Variations in the SAM explain up to ∼15% of the weekly rainfall variance in these regions, which is comparable to the variance accounted for by the El Niño–Southern Oscillation, especially during winter. The most widespread temperature anomalies associated with the SAM occur during the spring and summer seasons, when the high index polarity of the SAM is associated with anomalously low maximum temperature over most of central/eastern subtropical Australia. The regions of decreased maximum temperature are also associated with increased rainfall. Implications for recent trends in Australian rainfall and temperature are discussed.

Item Type: Article
Uncontrolled Keywords: annular mode,precipitation,surface temperature,southern hemisphere
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
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Depositing User: LivePure Connector
Date Deposited: 07 Jun 2022 11:30
Last Modified: 15 Jun 2023 04:33
URI: https://ueaeprints.uea.ac.uk/id/eprint/85390
DOI: 10.1175/JCLI4134.1

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