首页> 外文期刊>Hydrology Research >Analysis of hourly precipitation characteristics in Kraków, southern Poland, using a classification of circulation types
【24h】

Analysis of hourly precipitation characteristics in Kraków, southern Poland, using a classification of circulation types

机译:使用环流类型分类分析波兰南部克拉科夫的小时降水特征

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

This paper investigates the relationship between maximum precipitation in Krako ´w and typesnof atmospheric circulation in southern Poland, as classified by Niedz ´wiedz ´ . Three characteristicsnwere used to define this relationship: maximum precipitation (Pmax), its duration (d) andnprobability of exceedance ( p). The input data came from Krako ´w’s uniquely long andnhomogenous pluviographic record spanning the period 1886–2007. Hourly precipitation valuesnfor the maximum precipitation events were identified and arranged in 1–24 hour intervals. Theynwere then processed using the generalized extreme value (GEV) distribution to produce quantilesnof maximum precipitation totals in each of the intervals and broken down by the correspondingncirculation type. Differences between the development mechanisms are manifested innrelationships between precipitation characteristics and their measure of randomness,ni.e. exceedance probability. This paper demonstrates that maximum precipitation events dependnon their duration d and atmospheric circulation. The maximum short-duration (one-hour) eventsnoccur primarily in either of two circulation types: (i) cyclonic with advection from the east andnfrom the southeast or (ii) low-pressure centre and cyclonic trough. Maximum long-durationnprecipitation events (24 hour), on the other hand, occur in the cyclonic type of circulation withnadvection from the north and from the northeast.
机译:根据Niedz´wiedz的分类,本文研究了Krako´w的最大降水量与波兰南部大气环流类型之间的关系。定义了三种关系:最大降水量(Pmax),持续时间(d)和超概率(p)。输入的数据来自于1886-2007年间Krako'w独特而漫长的单相记录。确定最大降水事件的每小时降水值n,并以1–24小时为间隔进行排列。然后使用广义极值(GEV)分布处理该yn,以在每个间隔中产生最大降水总量的分位数,并按相应的循环类型进行分解。发展机制之间的差异表现为降水特征与其随机性度量之间的不相关性。超出概率。本文证明最大降水事件取决于其持续时间d和大气环流。最大的短时(一小时)事件主要发生在以下两种循环类型中的任何一种:(i)从东向平流,从东南向平流的旋风,或(ii)低压中心和旋风槽。另一方面,最大的长期降水事件(24小时)发生在从北部和东北方向对流的气旋型循环中。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号