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    Extratropical Cyclones in Idealized Simulations of Changed Climates

    Source: Journal of Climate:;2015:;volume( 028 ):;issue: 023::page 9373
    Author:
    Pfahl, Stephan
    ,
    O’Gorman, Paul A.
    ,
    Singh, Martin S.
    DOI: 10.1175/JCLI-D-14-00816.1
    Publisher: American Meteorological Society
    Abstract: yclones are a key element of extratropical weather and frequently lead to extreme events like wind storms and heavy precipitation. Understanding potential changes of cyclone frequency and intensity is thus essential for a proper assessment of climate change impacts. Here the behavior of extratropical cyclones under strongly varying climate conditions is investigated using idealized climate model simulations in an aquaplanet setup. A cyclone tracking algorithm is applied to assess various statistics of cyclone properties such as intensity, size, lifetime, displacement velocity, and deepening rates. In addition, a composite analysis of intense cyclones is performed. In general, the structure of extratropical cyclones in the idealized simulations is very robust, and changes in major cyclone characteristics are relatively small. Median cyclone intensity, measured in terms of minimum sea level pressure and lower-tropospheric relative vorticity, has a maximum in simulations with global mean temperature slightly warmer than present-day Earth, broadly consistent with the behavior of the eddy kinetic energy analyzed in previous studies. Maximum deepening rates along cyclone tracks behave similarly and are in agreement with linear quasigeostrophic growth rates if the effect of latent heat release on the stratification is taken into account. In contrast to moderate cyclones, the relative vorticity of intense cyclones continues to increase with warming to substantially higher temperatures, and this is associated with enhanced lower-tropospheric potential vorticity anomalies likely caused by increased diabatic heating. Moist processes may, therefore, lead to the further strengthening of intense cyclones in warmer climates even if cyclones weaken on average.
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      Extratropical Cyclones in Idealized Simulations of Changed Climates

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    contributor authorPfahl, Stephan
    contributor authorO’Gorman, Paul A.
    contributor authorSingh, Martin S.
    date accessioned2017-06-09T17:11:47Z
    date available2017-06-09T17:11:47Z
    date copyright2015/12/01
    date issued2015
    identifier issn0894-8755
    identifier otherams-80928.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4223874
    description abstractyclones are a key element of extratropical weather and frequently lead to extreme events like wind storms and heavy precipitation. Understanding potential changes of cyclone frequency and intensity is thus essential for a proper assessment of climate change impacts. Here the behavior of extratropical cyclones under strongly varying climate conditions is investigated using idealized climate model simulations in an aquaplanet setup. A cyclone tracking algorithm is applied to assess various statistics of cyclone properties such as intensity, size, lifetime, displacement velocity, and deepening rates. In addition, a composite analysis of intense cyclones is performed. In general, the structure of extratropical cyclones in the idealized simulations is very robust, and changes in major cyclone characteristics are relatively small. Median cyclone intensity, measured in terms of minimum sea level pressure and lower-tropospheric relative vorticity, has a maximum in simulations with global mean temperature slightly warmer than present-day Earth, broadly consistent with the behavior of the eddy kinetic energy analyzed in previous studies. Maximum deepening rates along cyclone tracks behave similarly and are in agreement with linear quasigeostrophic growth rates if the effect of latent heat release on the stratification is taken into account. In contrast to moderate cyclones, the relative vorticity of intense cyclones continues to increase with warming to substantially higher temperatures, and this is associated with enhanced lower-tropospheric potential vorticity anomalies likely caused by increased diabatic heating. Moist processes may, therefore, lead to the further strengthening of intense cyclones in warmer climates even if cyclones weaken on average.
    publisherAmerican Meteorological Society
    titleExtratropical Cyclones in Idealized Simulations of Changed Climates
    typeJournal Paper
    journal volume28
    journal issue23
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-14-00816.1
    journal fristpage9373
    journal lastpage9392
    treeJournal of Climate:;2015:;volume( 028 ):;issue: 023
    contenttypeFulltext
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