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    Statistics of the Global Tropopause Pressure

    Source: Monthly Weather Review:;1998:;volume( 126 ):;issue: 012::page 3303
    Author:
    Hoinka, Klaus P.
    DOI: 10.1175/1520-0493(1998)126<3303:SOTGTP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Statistics of the global tropopause pressure are evaluated for the period between 1979 and 1993. The analysis is based on gridded data as provided by the ECMWF reanalysis project. The thermal and dynamical definitions of the tropopause are applied in order to derive the surface separating the troposphere from the stratosphere. The dynamical tropopause is evaluated for threshhold values of potential vorticity of ±1.6, ±2.5, and ±3.5 potential vorticity units. Positive (negative) values are applied for the Northern (Southern) Hemisphere. The thermal tropopause is determined using the lapse-rate criteria. Frequency distributions of the tropopause pressure are shown above continental, ocean, polar, midlatitude, and tropical areas. Trends in the tropopause pressure are evaluated and compared with observed trends in total ozone.
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      Statistics of the Global Tropopause Pressure

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4204204
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    contributor authorHoinka, Klaus P.
    date accessioned2017-06-09T16:12:13Z
    date available2017-06-09T16:12:13Z
    date copyright1998/12/01
    date issued1998
    identifier issn0027-0644
    identifier otherams-63224.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4204204
    description abstractStatistics of the global tropopause pressure are evaluated for the period between 1979 and 1993. The analysis is based on gridded data as provided by the ECMWF reanalysis project. The thermal and dynamical definitions of the tropopause are applied in order to derive the surface separating the troposphere from the stratosphere. The dynamical tropopause is evaluated for threshhold values of potential vorticity of ±1.6, ±2.5, and ±3.5 potential vorticity units. Positive (negative) values are applied for the Northern (Southern) Hemisphere. The thermal tropopause is determined using the lapse-rate criteria. Frequency distributions of the tropopause pressure are shown above continental, ocean, polar, midlatitude, and tropical areas. Trends in the tropopause pressure are evaluated and compared with observed trends in total ozone.
    publisherAmerican Meteorological Society
    titleStatistics of the Global Tropopause Pressure
    typeJournal Paper
    journal volume126
    journal issue12
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1998)126<3303:SOTGTP>2.0.CO;2
    journal fristpage3303
    journal lastpage3325
    treeMonthly Weather Review:;1998:;volume( 126 ):;issue: 012
    contenttypeFulltext
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