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    Teleconnection between NAO and Climate Downstream of the Tibetan Plateau

    Source: Journal of Climate:;2008:;volume( 021 ):;issue: 018::page 4680
    Author:
    Li, Jian
    ,
    Yu, Rucong
    ,
    Zhou, Tianjun
    DOI: 10.1175/2008JCLI2053.1
    Publisher: American Meteorological Society
    Abstract: Analysis of the monthly NCEP?NCAR reanalysis data and station data reveals a teleconnection pattern (NAULEA) that links climate changes over the North Atlantic and Eurasia. The NAULEA pattern has five action centers. It extends from the North Atlantic to northwestern Europe, and then stretches eastward to the Urals, with its eastern end over North China. Certain climate changes over East Asia, such as the cooling changes in both the upper troposphere and surface in the last few decades of the twentieth century, can be attributed to the NAULEA pattern anomalies and traced upstream to the North Atlantic. The NAULEA pattern is suggested to be another NAO-related teleconnection pattern. Compared with the pattern with the Asian jet waveguide path, which leads to temperature anomalies over northeastern Asia, the NAULEA pattern with a high-latitude path exerts stronger influences on the climate of southwestern China.
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      Teleconnection between NAO and Climate Downstream of the Tibetan Plateau

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4208389
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    contributor authorLi, Jian
    contributor authorYu, Rucong
    contributor authorZhou, Tianjun
    date accessioned2017-06-09T16:23:25Z
    date available2017-06-09T16:23:25Z
    date copyright2008/09/01
    date issued2008
    identifier issn0894-8755
    identifier otherams-66992.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208389
    description abstractAnalysis of the monthly NCEP?NCAR reanalysis data and station data reveals a teleconnection pattern (NAULEA) that links climate changes over the North Atlantic and Eurasia. The NAULEA pattern has five action centers. It extends from the North Atlantic to northwestern Europe, and then stretches eastward to the Urals, with its eastern end over North China. Certain climate changes over East Asia, such as the cooling changes in both the upper troposphere and surface in the last few decades of the twentieth century, can be attributed to the NAULEA pattern anomalies and traced upstream to the North Atlantic. The NAULEA pattern is suggested to be another NAO-related teleconnection pattern. Compared with the pattern with the Asian jet waveguide path, which leads to temperature anomalies over northeastern Asia, the NAULEA pattern with a high-latitude path exerts stronger influences on the climate of southwestern China.
    publisherAmerican Meteorological Society
    titleTeleconnection between NAO and Climate Downstream of the Tibetan Plateau
    typeJournal Paper
    journal volume21
    journal issue18
    journal titleJournal of Climate
    identifier doi10.1175/2008JCLI2053.1
    journal fristpage4680
    journal lastpage4690
    treeJournal of Climate:;2008:;volume( 021 ):;issue: 018
    contenttypeFulltext
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