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    Source: Journal of Climate:;2017:;volume( 030 ):;issue: 010::page 3771
    Author:
    Chen, Shangfeng;Wu, Renguang
    DOI: 10.1175/JCLI-D-16-0477.1
    Publisher: American Meteorological Society
    Abstract: AbstractThis study investigates interdecadal changes in the relationship between interannual variations of boreal spring sea surface temperature (SST) in the North Atlantic and surface air temperature (SAT) over the mid-to-high latitudes of Eurasia during 1948?2014. Analyses show that the connection between the spring North Atlantic tripole SST anomaly pattern and the Eurasian SAT anomalies has experienced marked interdecadal shifts around the early 1970s and mid-1990s. The connection is strong during 1954?72 and 1996?2014 but weak during 1973?91. A diagnosis indicates that interdecadal changes in the connection between the North Atlantic SST and Eurasian SAT variations are associated with changes in atmospheric circulation anomalies over Eurasia induced by the North Atlantic tripole SST anomaly pattern. Further analyses suggest that changes in atmospheric circulation anomalies over Eurasia are related to changes in the position of atmospheric heating anomalies over the North Atlantic, which may be due to the change in mean SST. Marked atmospheric heating anomalies appear over the tropical western North Atlantic during 1954?72 and 1996?2014 but over the subtropical central-eastern North Atlantic during 1973?91. Barotropic model experiments confirm that different background flows may also contribute to changes in anomalous atmospheric circulation over Eurasia.
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    contributor authorChen, Shangfeng;Wu, Renguang
    date accessioned2018-01-03T11:00:43Z
    date available2018-01-03T11:00:43Z
    date copyright2/20/2017 12:00:00 AM
    date issued2017
    identifier otherjcli-d-16-0477.1.pdf
    identifier urihttp://138.201.223.254:8080/yetl1/handle/yetl/4246009
    description abstractAbstractThis study investigates interdecadal changes in the relationship between interannual variations of boreal spring sea surface temperature (SST) in the North Atlantic and surface air temperature (SAT) over the mid-to-high latitudes of Eurasia during 1948?2014. Analyses show that the connection between the spring North Atlantic tripole SST anomaly pattern and the Eurasian SAT anomalies has experienced marked interdecadal shifts around the early 1970s and mid-1990s. The connection is strong during 1954?72 and 1996?2014 but weak during 1973?91. A diagnosis indicates that interdecadal changes in the connection between the North Atlantic SST and Eurasian SAT variations are associated with changes in atmospheric circulation anomalies over Eurasia induced by the North Atlantic tripole SST anomaly pattern. Further analyses suggest that changes in atmospheric circulation anomalies over Eurasia are related to changes in the position of atmospheric heating anomalies over the North Atlantic, which may be due to the change in mean SST. Marked atmospheric heating anomalies appear over the tropical western North Atlantic during 1954?72 and 1996?2014 but over the subtropical central-eastern North Atlantic during 1973?91. Barotropic model experiments confirm that different background flows may also contribute to changes in anomalous atmospheric circulation over Eurasia.
    publisherAmerican Meteorological Society
    typeJournal Paper
    journal volume30
    journal issue10
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-16-0477.1
    journal fristpage3771
    journal lastpage3787
    treeJournal of Climate:;2017:;volume( 030 ):;issue: 010
    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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