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    The Signature of the Annular Modes in the Tropical Troposphere

    Source: Journal of Climate:;2004:;volume( 017 ):;issue: 022::page 4330
    Author:
    Thompson, David W. J.
    ,
    Lorenz, David J.
    DOI: 10.1175/3193.1
    Publisher: American Meteorological Society
    Abstract: The extratropical annular modes are coupled with a distinct pattern of climate anomalies that spans the circulation of the tropical troposphere. The signature of the annular modes in the tropical troposphere exhibits a high degree of equatorial symmetry. It is associated with upper-tropospheric zonal wind anomalies centered about the equator, midtropospheric temperature anomalies located ?20°N and 20°S, and opposing mean meridional circulation anomalies that span the subtropics of both hemispheres. The linkages between the annular modes and the tropical circulation are only evident during the cold season months, and are most robust in association with the Northern Hemisphere annular mode (NAM). The coupling between the annular modes and the circulation of the tropical troposphere is consistent with forcing by waves originating at extratropical latitudes. Both annular modes are characterized by anomalies in the eddy momentum flux convergence at tropical latitudes that act to reinforce the changes in the tropical wind and temperature fields. The most pronounced tropical anomalies lag indices of the annular modes by ?2 weeks and are found over the eastern tropical Pacific, where climatological westerlies permit extratropical waves to propagate into the deep Tropics. The linkages between the NAM and the tropical tropospheric circulation are most pronounced during the cold phase of the El Niño?Southern Oscillation cycle. The recent trend in the NAM is linearly congruent with a ?0.1-K cooling of the tropical troposphere over the past two decades during the Northern Hemisphere winter season.
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      The Signature of the Annular Modes in the Tropical Troposphere

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4214369
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    contributor authorThompson, David W. J.
    contributor authorLorenz, David J.
    date accessioned2017-06-09T16:41:42Z
    date available2017-06-09T16:41:42Z
    date copyright2004/11/01
    date issued2004
    identifier issn0894-8755
    identifier otherams-72373.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4214369
    description abstractThe extratropical annular modes are coupled with a distinct pattern of climate anomalies that spans the circulation of the tropical troposphere. The signature of the annular modes in the tropical troposphere exhibits a high degree of equatorial symmetry. It is associated with upper-tropospheric zonal wind anomalies centered about the equator, midtropospheric temperature anomalies located ?20°N and 20°S, and opposing mean meridional circulation anomalies that span the subtropics of both hemispheres. The linkages between the annular modes and the tropical circulation are only evident during the cold season months, and are most robust in association with the Northern Hemisphere annular mode (NAM). The coupling between the annular modes and the circulation of the tropical troposphere is consistent with forcing by waves originating at extratropical latitudes. Both annular modes are characterized by anomalies in the eddy momentum flux convergence at tropical latitudes that act to reinforce the changes in the tropical wind and temperature fields. The most pronounced tropical anomalies lag indices of the annular modes by ?2 weeks and are found over the eastern tropical Pacific, where climatological westerlies permit extratropical waves to propagate into the deep Tropics. The linkages between the NAM and the tropical tropospheric circulation are most pronounced during the cold phase of the El Niño?Southern Oscillation cycle. The recent trend in the NAM is linearly congruent with a ?0.1-K cooling of the tropical troposphere over the past two decades during the Northern Hemisphere winter season.
    publisherAmerican Meteorological Society
    titleThe Signature of the Annular Modes in the Tropical Troposphere
    typeJournal Paper
    journal volume17
    journal issue22
    journal titleJournal of Climate
    identifier doi10.1175/3193.1
    journal fristpage4330
    journal lastpage4342
    treeJournal of Climate:;2004:;volume( 017 ):;issue: 022
    contenttypeFulltext
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