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Precipitation variability in the Meuse basin in relation to atmospheric circulation

机译:默兹盆地降水变化与大气环流的关系

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摘要

The distribution of precipitation events in the Meuse basin during the past century has been found to reflect the large-scale atmospheric circulation, as characterised by the Grosswetterlagen system. Statistical analysis of the long observation records (1911-2002) for the basin showed that although the annual (November to October) and winter half-year (November to April) frequencies of wet days (>= 1 mm/day) were nearly stable, the associated precipitation amounts have significantly increased since 1980. From 1980 onwards, the very wet days (>= 10 mm/day) in the winter half-year have become more frequent. No obvious change was identified for the summer half-year (May to October) very wet days. Both the precipitation amounts of wet and very wet days in the winter half-year and the occurrence of associated atmospheric circulation of the types/sub-types west cyclone, southwest cyclone and northwest cyclone showed a significant increase around 1980.
机译:过去一个世纪以来,默兹盆地的降水事件分布被发现反映了大气压环流,以大格特维根系统为特征。对盆地长期观测记录(1911-2002年)的统计分析表明,尽管每年(十一月至十月)和冬季半年(十一月至四月)的湿天频率(> = 1毫米/天)几乎稳定自1980年以来,相关的降水量显着增加。从1980年开始,冬季半年中的非常潮湿的日子(> = 10毫米/天)变得更加频繁。在非常潮湿的夏季半年(5月至10月),没有发现明显的变化。在冬季半年中,潮湿和非常潮湿的日子的降水量以及西气旋,西南气旋和西北气旋类型/亚型的相关大气环流的发生都在1980年前后显着增加。

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