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Title: Teleconnection between Australian winter temperature and Indian summer monsoon rainfall
Authors: Lee, Soo-Ying
Koh, Tieh Yong
Issue Date: 2012
Source: Lee, S. Y., & Koh, T. Y. (2012). Teleconnection between Australian winter temperature and Indian summer monsoon rainfall. Atmospheric Chemistry and Physics, 12, 669-681.
Series/Report no.: Atmospheric chemistry and physics
Abstract: The pattern of evaporative sources and the direction of the large-scale circulation over the Indian Ocean during the boreal summer raises the question of whether atmospheric conditions in Australia could influence conditions over the Indian subcontinent, despite the long passage of air over the Indian Ocean. The authors propose that such an influence is sometimes possible when there is unusually low temperature over inland Australia during the austral winter, through the mechanism where such a temperature extreme enhances evaporation rate over the eastern tropical Indian Ocean and hence enhances rainfall over two regions in western India after 13–19 days. Results from trajectory calculations indicate that such an influence is mechanistically feasible, with air of Australian origin contributing 0.5–1.5% of the climatological net precipitation for monsoon seasonal rainfall over western India. Statistics performed on reanalysis, satellite and in situ data are consistent with such a mechanism. Since extreme winter temperature in Australia is often associated with cold-air outbreaks, the described mechanism may be an example of how southern hemispheric mid-latitude weather can influence northern hemispheric monsoon rainfall. Further study is recommended through modelling and comparison with various known causes of atmospheric variability to confirm the existence of such a mechanism and determine the extent of its influence during specific low temperature episodes.
DOI: 10.5194/acp-12-669-2012
Rights: © 2012 The Authors. This paper was published in Atmospheric Chemistry and Physics and is made available as an electronic reprint (preprint) with permission of The Authors. The paper can be found at the following official DOI: []. One print or electronic copy may be made for personal use only. Systematic or multiple reproduction, distribution to multiple locations via electronic or other means, duplication of any material in this paper for a fee or for commercial purposes, or modification of the content of the paper is prohibited and is subject to penalties under law.
Fulltext Permission: open
Fulltext Availability: With Fulltext
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