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    A Possible Influence of Equatorial Winds on the September 2002 Southern Hemisphere Sudden Warming Event

    Source: Journal of the Atmospheric Sciences:;2005:;Volume( 062 ):;issue: 003::page 651
    Author:
    Gray, Lesley
    ,
    Norton, Warwick
    ,
    Pascoe, Charlotte
    ,
    Charlton, Andrew
    DOI: 10.1175/JAS-3339.1
    Publisher: American Meteorological Society
    Abstract: The stratospheric sudden warming in the Southern Hemisphere (SH) in September 2002 was unexpected for two reasons. First, planetary wave activity in the Southern Hemisphere is very weak, and midwinter warmings have never been observed, at least not since observations of the upper stratosphere became regularly available. Second, the warming occurred in a west phase of the quasi-biennial oscillation (QBO) in the lower stratosphere. This is unexpected because warmings are usually considered to be more likely in the east phase of the QBO, when a zero wind line is present in the winter subtropics and hence confines planetary wave propagation to higher latitudes closer to the polar vortex. At first, this evidence suggests that the sudden warming must therefore be simply a result of anomalously strong planetary wave forcing from the troposphere. However, recent model studies have suggested that the midwinter polar vortex may also be sensitive to the equatorial winds in the upper stratosphere, the region dominated by the semiannual oscillation. In this paper, the time series of equatorial zonal winds from two different data sources, the 40-yr ECMWF Re-Analysis (ERA) and the Met Office assimilated dataset, are reviewed. Both suggest that the equatorial winds in the upper stratosphere above 10 hPa were anomalously easterly in 2002. Idealized model experiments are described in which the modeled equatorial winds were relaxed toward these observations for various years to examine whether the anomalous easterlies in 2002 could influence the timing of a warming event. It is found that the 2002 equatorial winds speed up the evolution of a warming event in the model. Therefore, this study suggests that the anomalous easterlies in the 1?10-hPa region may have been a contributory factor in the development of the observed SH warming. However, it is concluded that it is unlikely that the anomalous equatorial winds alone can explain the 2002 warming event.
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      A Possible Influence of Equatorial Winds on the September 2002 Southern Hemisphere Sudden Warming Event

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4217875
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    • Journal of the Atmospheric Sciences

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    contributor authorGray, Lesley
    contributor authorNorton, Warwick
    contributor authorPascoe, Charlotte
    contributor authorCharlton, Andrew
    date accessioned2017-06-09T16:51:55Z
    date available2017-06-09T16:51:55Z
    date copyright2005/03/01
    date issued2005
    identifier issn0022-4928
    identifier otherams-75529.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4217875
    description abstractThe stratospheric sudden warming in the Southern Hemisphere (SH) in September 2002 was unexpected for two reasons. First, planetary wave activity in the Southern Hemisphere is very weak, and midwinter warmings have never been observed, at least not since observations of the upper stratosphere became regularly available. Second, the warming occurred in a west phase of the quasi-biennial oscillation (QBO) in the lower stratosphere. This is unexpected because warmings are usually considered to be more likely in the east phase of the QBO, when a zero wind line is present in the winter subtropics and hence confines planetary wave propagation to higher latitudes closer to the polar vortex. At first, this evidence suggests that the sudden warming must therefore be simply a result of anomalously strong planetary wave forcing from the troposphere. However, recent model studies have suggested that the midwinter polar vortex may also be sensitive to the equatorial winds in the upper stratosphere, the region dominated by the semiannual oscillation. In this paper, the time series of equatorial zonal winds from two different data sources, the 40-yr ECMWF Re-Analysis (ERA) and the Met Office assimilated dataset, are reviewed. Both suggest that the equatorial winds in the upper stratosphere above 10 hPa were anomalously easterly in 2002. Idealized model experiments are described in which the modeled equatorial winds were relaxed toward these observations for various years to examine whether the anomalous easterlies in 2002 could influence the timing of a warming event. It is found that the 2002 equatorial winds speed up the evolution of a warming event in the model. Therefore, this study suggests that the anomalous easterlies in the 1?10-hPa region may have been a contributory factor in the development of the observed SH warming. However, it is concluded that it is unlikely that the anomalous equatorial winds alone can explain the 2002 warming event.
    publisherAmerican Meteorological Society
    titleA Possible Influence of Equatorial Winds on the September 2002 Southern Hemisphere Sudden Warming Event
    typeJournal Paper
    journal volume62
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/JAS-3339.1
    journal fristpage651
    journal lastpage667
    treeJournal of the Atmospheric Sciences:;2005:;Volume( 062 ):;issue: 003
    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