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首页> 外文期刊>Theoretical and applied climatology >Variability of high rainfalls and related synoptic situations causing heavy floods at the northern foothills of the Tatra Mountains
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Variability of high rainfalls and related synoptic situations causing heavy floods at the northern foothills of the Tatra Mountains

机译:塔特拉山北部山麓高降雨和相关天气状况的变化导致大洪水

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摘要

This contribution provides the basics of the climatology of the Polish Tatra Mountains in a nutshell, with particular reference to intense precipitation and its relation to atmospheric circulation. Variability of various precipitation characteristics, including selected indices of intense precipitation in Zakopane and at Kasprowy Wierch, is illustrated in this paper. None of the trends in these characteristics and indices calculated for the entire time interval exhibit a statistical significance, but short-time fluctuations are evident. The occurrence of intense precipitation in the Tatra Mountains is strongly related to three circulation types. These situations (Nc, NEc, Bc) are associated with cyclones following track Vb after van Bebber. In addition to changing frequencies of circulation, this study also reveals an increase in the frequency of the circulation types associated with extreme precipitation.
机译:简而言之,该贡献为波兰塔特拉山的气候学提供了基础,特别是关于强降水及其与大气环流的关系。本文说明了各种降水特征的变化,包括扎科帕内和卡斯普罗维耶(Kasprowy Wierch)强降水的选定指标。在整个时间间隔内计算出的这些特征和指数的趋势都没有统计学意义,但是短期波动是明显的。塔特拉山中强降水的发生与三种循环类型密切相关。这些情况(Nc,NEc,Bc)与范贝伯之后跟随轨道Vb的气旋有关。除了改变循环频率外,这项研究还揭示了与极端降水有关的循环类型频率的增加。

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  • 来源
    《Theoretical and applied climatology》 |2015年第2期|273-284|共12页
  • 作者单位

    Faculty of Earth Sciences, University of Silesia, Sosnowiec, Poland;

    Faculty of Earth Sciences, University of Silesia, Sosnowiec, Poland;

    Institute for Agricultural and Forest Environment, Polish Academy of Sciences, Poznan, Poland;

    Institute for Agricultural and Forest Environment, Polish Academy of Sciences, Poznan, Poland;

    Dendrolab.ch, Institute of Geological Sciences, University of Bern, Bern, Switzerland,Institute for Environmental Sciences, University of Geneva, Geneva, Switzerland;

    Faculty of Earth Sciences, University of Silesia, Sosnowiec, Poland;

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