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    The Impacts of Multiscale Weather Systems on Freezing Rain and Snowstorms over Southern China

    Source: Weather and Forecasting:;2009:;volume( 025 ):;issue: 002::page 388
    Author:
    Sun, Jianhua
    ,
    Zhao, Sixiong
    DOI: 10.1175/2009WAF2222253.1
    Publisher: American Meteorological Society
    Abstract: This paper investigated the interactions between the synoptic patterns, quasi-stationary fronts, eastward-propagating cloud clusters from the Tibetan Plateau, surface conditions, and atmospheric stratification processes associated with a 20-day event of freezing precipitation over southern China from January to February 2008. It was found that the long duration of the freezing precipitation process was primarily caused by stationary and anomalous synoptic weather patterns such as a blocking high pressure system in the northern branch and a trough in the south branch of the westerlies, which resulted in the convergence of cold air from northern China and warm, moist air from the south. The cloud clusters over the Tibetan Plateau propagated eastward and showed noticeable impacts in the local areas when they moved over southern China during several similar cloud propagation processes from January to February 2008. An east?west-oriented quasi-stationary front system in southern China, which is rare during the Asian winter monsoon season, is responsible for producing freezing precipitation and snowstorms. A stronger horizontal gradient of the isolines of the pseudo-equivalent potential temperature and higher temperatures at the inversion layer in the western part of the front than that in its eastern part can be found. At the same time, low-level moisture convergence ahead of the front enhanced the formation, development, and persistence of freezing precipitation in the west part of the front. The thickness of the warm layer and the temperature inversion layer also modulated the intensity and duration of freezing rain and ice pellets. Temperature from about ?1° to ?3°C and weak winds were found to be favorable meteorological factors at the surface level for freezing precipitation. These analysis results are synthesized into a conceptual model that coherently describes the physics processes associated with the synoptic features and quasi-stationary front system as well as the atmospheric stratification process during the freezing precipitation event.
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      The Impacts of Multiscale Weather Systems on Freezing Rain and Snowstorms over Southern China

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4211452
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    contributor authorSun, Jianhua
    contributor authorZhao, Sixiong
    date accessioned2017-06-09T16:32:48Z
    date available2017-06-09T16:32:48Z
    date copyright2010/04/01
    date issued2009
    identifier issn0882-8156
    identifier otherams-69749.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4211452
    description abstractThis paper investigated the interactions between the synoptic patterns, quasi-stationary fronts, eastward-propagating cloud clusters from the Tibetan Plateau, surface conditions, and atmospheric stratification processes associated with a 20-day event of freezing precipitation over southern China from January to February 2008. It was found that the long duration of the freezing precipitation process was primarily caused by stationary and anomalous synoptic weather patterns such as a blocking high pressure system in the northern branch and a trough in the south branch of the westerlies, which resulted in the convergence of cold air from northern China and warm, moist air from the south. The cloud clusters over the Tibetan Plateau propagated eastward and showed noticeable impacts in the local areas when they moved over southern China during several similar cloud propagation processes from January to February 2008. An east?west-oriented quasi-stationary front system in southern China, which is rare during the Asian winter monsoon season, is responsible for producing freezing precipitation and snowstorms. A stronger horizontal gradient of the isolines of the pseudo-equivalent potential temperature and higher temperatures at the inversion layer in the western part of the front than that in its eastern part can be found. At the same time, low-level moisture convergence ahead of the front enhanced the formation, development, and persistence of freezing precipitation in the west part of the front. The thickness of the warm layer and the temperature inversion layer also modulated the intensity and duration of freezing rain and ice pellets. Temperature from about ?1° to ?3°C and weak winds were found to be favorable meteorological factors at the surface level for freezing precipitation. These analysis results are synthesized into a conceptual model that coherently describes the physics processes associated with the synoptic features and quasi-stationary front system as well as the atmospheric stratification process during the freezing precipitation event.
    publisherAmerican Meteorological Society
    titleThe Impacts of Multiscale Weather Systems on Freezing Rain and Snowstorms over Southern China
    typeJournal Paper
    journal volume25
    journal issue2
    journal titleWeather and Forecasting
    identifier doi10.1175/2009WAF2222253.1
    journal fristpage388
    journal lastpage407
    treeWeather and Forecasting:;2009:;volume( 025 ):;issue: 002
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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