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    Is Pacific Storm-Track Activity Correlated with the Strength of Upstream Wave Seeding?

    Source: Journal of Climate:;2012:;volume( 025 ):;issue: 017::page 5768
    Author:
    Chang, Edmund K. M.
    ,
    Guo, Yanjuan
    DOI: 10.1175/JCLI-D-11-00555.1
    Publisher: American Meteorological Society
    Abstract: n this paper, the relationship between upstream seeding over north Asia and downstream storm-track activity over the North Pacific in midwinter and spring/fall has been analyzed using 45 years of variance and feature-tracking statistics. It is shown that for each season, interannual variations in upstream seeding and downstream storm-track activity are largely uncorrelated. Moreover, during midwinter months in which the upstream seeding from north Asia is about as strong as that during a typical spring/fall month, the downstream storm track in central Pacific is still significantly weaker during midwinter than that during spring/fall. In addition, during cool seasons in which the midwinter suppression is more pronounced in the upstream seeding region, the suppression is not significantly enhanced in the downstream Pacific storm track.A recent study suggested that reduced upstream seeding from north Asia is the main ?source? of the midwinter suppression of the Pacific storm track. Results presented in this study suggest that it is unlikely that the weakness in upstream seeding is the primary cause of the midwinter suppression.
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      Is Pacific Storm-Track Activity Correlated with the Strength of Upstream Wave Seeding?

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    contributor authorChang, Edmund K. M.
    contributor authorGuo, Yanjuan
    date accessioned2017-06-09T17:05:20Z
    date available2017-06-09T17:05:20Z
    date copyright2012/09/01
    date issued2012
    identifier issn0894-8755
    identifier otherams-79203.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4221958
    description abstractn this paper, the relationship between upstream seeding over north Asia and downstream storm-track activity over the North Pacific in midwinter and spring/fall has been analyzed using 45 years of variance and feature-tracking statistics. It is shown that for each season, interannual variations in upstream seeding and downstream storm-track activity are largely uncorrelated. Moreover, during midwinter months in which the upstream seeding from north Asia is about as strong as that during a typical spring/fall month, the downstream storm track in central Pacific is still significantly weaker during midwinter than that during spring/fall. In addition, during cool seasons in which the midwinter suppression is more pronounced in the upstream seeding region, the suppression is not significantly enhanced in the downstream Pacific storm track.A recent study suggested that reduced upstream seeding from north Asia is the main ?source? of the midwinter suppression of the Pacific storm track. Results presented in this study suggest that it is unlikely that the weakness in upstream seeding is the primary cause of the midwinter suppression.
    publisherAmerican Meteorological Society
    titleIs Pacific Storm-Track Activity Correlated with the Strength of Upstream Wave Seeding?
    typeJournal Paper
    journal volume25
    journal issue17
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-11-00555.1
    journal fristpage5768
    journal lastpage5776
    treeJournal of Climate:;2012:;volume( 025 ):;issue: 017
    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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