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    Assessing the Influence of Regional SST Modes on the Winter Temperature in China: The Effect of Tropical Pacific and Atlantic

    Source: Journal of Climate:;2013:;volume( 027 ):;issue: 002::page 868
    Author:
    Jiang, Zhihong
    ,
    Yang, Hao
    ,
    Liu, Zhengyu
    ,
    Wu, Yanzhu
    ,
    Wen, Na
    DOI: 10.1175/JCLI-D-12-00847.1
    Publisher: American Meteorological Society
    Abstract: his study investigates the influence of different sea surface temperature (SST) modes on the winter temperature in China using the generalized equilibrium feedback assessment (GEFA). It is found that the second EOF mode of winter temperature in China during 1958?2010 shows a typical northeast?southwest (NE?SW) pattern, which is a major spatial mode of Chinese winter temperature at interannual scales. The winter temperature of the NE?SW pattern is forced mainly by SST modes in the tropical Pacific and Atlantic. For 2009/10, the tropical Pacific El Niño mode and tropical Atlantic tripole mode have the largest contribution to the response. The physical mechanism of the cold northeast?warm southwest (CNE?WSW) pattern is also explained in terms of GEFA of the responses of the atmospheric circulation. The northerly flow at the low level transports cold air to northern and northeastern China, resulting in a lower temperature there. Meanwhile, the anomaly meridional wind advects warm air from the southern oceans to southwestern China, leading to warming there.
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      Assessing the Influence of Regional SST Modes on the Winter Temperature in China: The Effect of Tropical Pacific and Atlantic

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4222734
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    contributor authorJiang, Zhihong
    contributor authorYang, Hao
    contributor authorLiu, Zhengyu
    contributor authorWu, Yanzhu
    contributor authorWen, Na
    date accessioned2017-06-09T17:08:05Z
    date available2017-06-09T17:08:05Z
    date copyright2014/01/01
    date issued2013
    identifier issn0894-8755
    identifier otherams-79902.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4222734
    description abstracthis study investigates the influence of different sea surface temperature (SST) modes on the winter temperature in China using the generalized equilibrium feedback assessment (GEFA). It is found that the second EOF mode of winter temperature in China during 1958?2010 shows a typical northeast?southwest (NE?SW) pattern, which is a major spatial mode of Chinese winter temperature at interannual scales. The winter temperature of the NE?SW pattern is forced mainly by SST modes in the tropical Pacific and Atlantic. For 2009/10, the tropical Pacific El Niño mode and tropical Atlantic tripole mode have the largest contribution to the response. The physical mechanism of the cold northeast?warm southwest (CNE?WSW) pattern is also explained in terms of GEFA of the responses of the atmospheric circulation. The northerly flow at the low level transports cold air to northern and northeastern China, resulting in a lower temperature there. Meanwhile, the anomaly meridional wind advects warm air from the southern oceans to southwestern China, leading to warming there.
    publisherAmerican Meteorological Society
    titleAssessing the Influence of Regional SST Modes on the Winter Temperature in China: The Effect of Tropical Pacific and Atlantic
    typeJournal Paper
    journal volume27
    journal issue2
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-12-00847.1
    journal fristpage868
    journal lastpage879
    treeJournal of Climate:;2013:;volume( 027 ):;issue: 002
    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
    yabeshDSpacePersian