Circulation background of the atmospheric precipitation in Central Europe (based on the Polish example)

The influence of circulation upon the atmospheric precipitation in Poland as an example of Central European climatic conditions is analysed. The study is based on daily sums of precipitation which have been collected from over 50 meteorological stations for the period of 1951-1999 as well as on Groß...

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Main Authors: Zbigniew Ustrnul, Danuta Czekierda
Format: Article
Language:English
Published: Borntraeger 2001-04-01
Series:Meteorologische Zeitschrift
Online Access:http://dx.doi.org/10.1127/0941-2948/2001/0010-0103
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spelling doaj-a3f8cc4db66b480eb013cf88f05834b52020-11-24T23:28:21ZengBorntraegerMeteorologische Zeitschrift0941-29482001-04-0110210311110.1127/0941-2948/2001/0010-010349096Circulation background of the atmospheric precipitation in Central Europe (based on the Polish example)Zbigniew UstrnulDanuta CzekierdaThe influence of circulation upon the atmospheric precipitation in Poland as an example of Central European climatic conditions is analysed. The study is based on daily sums of precipitation which have been collected from over 50 meteorological stations for the period of 1951-1999 as well as on Großwetterlagen circulation patterns. The analysis confirms the considerable influence of atmospheric circulation upon precipitation totals and especially upon their extreme values. The highest rainfalls occur during situations with N-NE-E air flow. During these circulation types and cyclonic troughs or with the cyclonic centre over Central Europe the highest probability of high daily totals is usually observed. However, heavy rainfalls in summer can also occur during other situations even including those with high pressure. Obviously these circulation patterns also have the highest chance for days without any precipitation as well as the lowest mean daily totals. A climatological analysis of the seasonal and annual precipitation totals associated with circulation indices confirmed relatively close connections between these variables.http://dx.doi.org/10.1127/0941-2948/2001/0010-0103
collection DOAJ
language English
format Article
sources DOAJ
author Zbigniew Ustrnul
Danuta Czekierda
spellingShingle Zbigniew Ustrnul
Danuta Czekierda
Circulation background of the atmospheric precipitation in Central Europe (based on the Polish example)
Meteorologische Zeitschrift
author_facet Zbigniew Ustrnul
Danuta Czekierda
author_sort Zbigniew Ustrnul
title Circulation background of the atmospheric precipitation in Central Europe (based on the Polish example)
title_short Circulation background of the atmospheric precipitation in Central Europe (based on the Polish example)
title_full Circulation background of the atmospheric precipitation in Central Europe (based on the Polish example)
title_fullStr Circulation background of the atmospheric precipitation in Central Europe (based on the Polish example)
title_full_unstemmed Circulation background of the atmospheric precipitation in Central Europe (based on the Polish example)
title_sort circulation background of the atmospheric precipitation in central europe (based on the polish example)
publisher Borntraeger
series Meteorologische Zeitschrift
issn 0941-2948
publishDate 2001-04-01
description The influence of circulation upon the atmospheric precipitation in Poland as an example of Central European climatic conditions is analysed. The study is based on daily sums of precipitation which have been collected from over 50 meteorological stations for the period of 1951-1999 as well as on Großwetterlagen circulation patterns. The analysis confirms the considerable influence of atmospheric circulation upon precipitation totals and especially upon their extreme values. The highest rainfalls occur during situations with N-NE-E air flow. During these circulation types and cyclonic troughs or with the cyclonic centre over Central Europe the highest probability of high daily totals is usually observed. However, heavy rainfalls in summer can also occur during other situations even including those with high pressure. Obviously these circulation patterns also have the highest chance for days without any precipitation as well as the lowest mean daily totals. A climatological analysis of the seasonal and annual precipitation totals associated with circulation indices confirmed relatively close connections between these variables.
url http://dx.doi.org/10.1127/0941-2948/2001/0010-0103
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