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    Possible Role of the Indian Ocean in the In-Phase Transition of the Indian-to-Australian Summer Monsoon

    Source: Journal of Climate:;2008:;volume( 021 ):;issue: 021::page 5727
    Author:
    Wu, Renguang
    DOI: 10.1175/2008JCLI2354.1
    Publisher: American Meteorological Society
    Abstract: Analysis of observations shows that in-phase transitions from the Indian summer monsoon (ISM) to the Australian summer monsoon (ASM) have occurred both in El Niño?Southern Oscillation (ENSO) and non-ENSO years. The present study investigates possible roles of the Indian Ocean in the in-phase ISM-to-ASM transitions. It is shown that an anomalous ISM leads to sea surface temperature (SST) anomalies in the tropical Indian Ocean through wind?evaporation effects. The resultant Indian Ocean SST anomalies induce an anomalous ASM of the same sign as the ISM through an anomalous east?west circulation over the eastern Indian Ocean and the Maritime Continent?northern Australia. The results indicate that the in-phase ISM-to-ASM transitions in non-ENSO years can be accomplished through monsoon?Indian Ocean interactions. The results of observational analysis are confirmed with numerical model experiments.
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      Possible Role of the Indian Ocean in the In-Phase Transition of the Indian-to-Australian Summer Monsoon

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4208573
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    contributor authorWu, Renguang
    date accessioned2017-06-09T16:23:57Z
    date available2017-06-09T16:23:57Z
    date copyright2008/11/01
    date issued2008
    identifier issn0894-8755
    identifier otherams-67157.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208573
    description abstractAnalysis of observations shows that in-phase transitions from the Indian summer monsoon (ISM) to the Australian summer monsoon (ASM) have occurred both in El Niño?Southern Oscillation (ENSO) and non-ENSO years. The present study investigates possible roles of the Indian Ocean in the in-phase ISM-to-ASM transitions. It is shown that an anomalous ISM leads to sea surface temperature (SST) anomalies in the tropical Indian Ocean through wind?evaporation effects. The resultant Indian Ocean SST anomalies induce an anomalous ASM of the same sign as the ISM through an anomalous east?west circulation over the eastern Indian Ocean and the Maritime Continent?northern Australia. The results indicate that the in-phase ISM-to-ASM transitions in non-ENSO years can be accomplished through monsoon?Indian Ocean interactions. The results of observational analysis are confirmed with numerical model experiments.
    publisherAmerican Meteorological Society
    titlePossible Role of the Indian Ocean in the In-Phase Transition of the Indian-to-Australian Summer Monsoon
    typeJournal Paper
    journal volume21
    journal issue21
    journal titleJournal of Climate
    identifier doi10.1175/2008JCLI2354.1
    journal fristpage5727
    journal lastpage5741
    treeJournal of Climate:;2008:;volume( 021 ):;issue: 021
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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