Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/104589
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dc.contributor.authorLee, Soo-Yingen
dc.contributor.authorKoh, Tieh Yongen
dc.date.accessioned2013-02-01T01:40:27Zen
dc.date.accessioned2019-12-06T21:35:48Z-
dc.date.available2013-02-01T01:40:27Zen
dc.date.available2019-12-06T21:35:48Z-
dc.date.copyright2011en
dc.date.issued2011en
dc.identifier.citationLee, S. Y., & Koh, T. Y. (2011). Teleconnection between Australian winter temperature and Indian summer monsoon rainfall. Atmospheric Chemistry and Physics Discussions, 11(9), 26415-26440.en
dc.identifier.issn1680-7375en
dc.identifier.urihttps://hdl.handle.net/10356/104589-
dc.description.abstractThe 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. Using a combination of reanalysis, satellite and in situ data, we argue that unusually low temperature over inland Australia during austral winter can enhance evaporation rate over the eastern tropical Indian Ocean, and hence enhance rainfall over western India after 10–18 days. Since extreme winter temperature in Australia is often associated with cold-air outbreaks, the above mechanism can be an example of how southern hemispheric mid-latitude weather can influence northern hemispheric monsoon rainfall.en
dc.language.isoenen
dc.relation.ispartofseriesAtmospheric chemistry and physics discussionsen
dc.rights© 2011 The Author(s).en
dc.subjectDRNTU::Science::Physics::Meteorology and climatologyen
dc.titleTeleconnection between Australian winter temperature and Indian summer monsoon rainfallen
dc.typeJournal Articleen
dc.contributor.schoolSchool of Physical and Mathematical Sciencesen
dc.contributor.researchEarth Observatory of Singaporeen
dc.identifier.doi10.5194/acpd-11-26415-2011en
dc.description.versionPublished versionen
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