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    Association of the Poleward Shift of East Asian Subtropical Upper-Level Jet with Frequent Tropical Cyclone Activities over the Western North Pacific in Summer

    Source: Journal of Climate:;2017:;volume( 030 ):;issue: 014::page 5597
    Author:
    Chen, Xian;Zhong, Zhong;Lu, Wei
    DOI: 10.1175/JCLI-D-16-0334.1
    Publisher: American Meteorological Society
    Abstract: AbstractThe NCEP?NCAR reanalysis dataset and the tropical cyclone (TC) best-track dataset from the Regional Specialized Meteorological Center (RSMC) Tokyo Typhoon Center were employed in the present study to investigate the possible linkage of the meridional displacement of the East Asian subtropical upper-level jet (EASJ) with the TC activity over the western North Pacific (WNP). Results indicate that summertime frequent TC activities would create the poleward shift of the EASJ through a stimulated Pacific?Japan (PJ) teleconnection pattern as well as the changed large-scale meridional temperature gradient. On the contrary, in the inactive TC years, the EASJ is often located more southward than normal with an enhanced intensity. Therefore, TC activities over the WNP are closely related to the location and intensity of the EASJ in summer at the interannual time scale.
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      Association of the Poleward Shift of East Asian Subtropical Upper-Level Jet with Frequent Tropical Cyclone Activities over the Western North Pacific in Summer

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    contributor authorChen, Xian;Zhong, Zhong;Lu, Wei
    date accessioned2018-01-03T11:00:28Z
    date available2018-01-03T11:00:28Z
    date copyright4/10/2017 12:00:00 AM
    date issued2017
    identifier otherjcli-d-16-0334.1.pdf
    identifier urihttp://138.201.223.254:8080/yetl1/handle/yetl/4245950
    description abstractAbstractThe NCEP?NCAR reanalysis dataset and the tropical cyclone (TC) best-track dataset from the Regional Specialized Meteorological Center (RSMC) Tokyo Typhoon Center were employed in the present study to investigate the possible linkage of the meridional displacement of the East Asian subtropical upper-level jet (EASJ) with the TC activity over the western North Pacific (WNP). Results indicate that summertime frequent TC activities would create the poleward shift of the EASJ through a stimulated Pacific?Japan (PJ) teleconnection pattern as well as the changed large-scale meridional temperature gradient. On the contrary, in the inactive TC years, the EASJ is often located more southward than normal with an enhanced intensity. Therefore, TC activities over the WNP are closely related to the location and intensity of the EASJ in summer at the interannual time scale.
    publisherAmerican Meteorological Society
    titleAssociation of the Poleward Shift of East Asian Subtropical Upper-Level Jet with Frequent Tropical Cyclone Activities over the Western North Pacific in Summer
    typeJournal Paper
    journal volume30
    journal issue14
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-16-0334.1
    journal fristpage5597
    journal lastpage5603
    treeJournal of Climate:;2017:;volume( 030 ):;issue: 014
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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