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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Trends in daily precipitation and temperature extremes across western Germany in the second half of the 20th century
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Trends in daily precipitation and temperature extremes across western Germany in the second half of the 20th century

机译:20世纪下半叶整个德国西部的每日降水和极端温度趋势

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The evolution of daily extreme precipitation and temperature from 1958 to 2001 was investigated within the German side of the Rhine basin. Trends of a set of extreme precipitation and temperature indices defined on daily time series of precipitation and temperature were calculated at 611 precipitation and 232 temperature stations located within the study area and their corresponding Significances were tested using the non-parametric Kendall- tau test. The results obtained indicated that both the daily minimum and maximum extreme temperatures have increased over the investigation period, with the degree of change showing seasonal variability. On an annual basis, the change in the daily minimum extreme temperature was found to be greater than that of the daily maximum extreme temperature. The daily extreme heavy precipitation has shown increasing trends both in magnitude and frequency of occurrence in all seasons except summer, where it showed the opposite trend. The station values of the daily precipitation were also interpolated on a regular grid of 5 km x 5 km so that the changes in the indices could be investigated on areal precipitation by aggregating the interpolated precipitation to any desired scale. This enables assessment of the hydrological consequences of the changes in the extreme precipitation. Although the spatial pattern remained more or less similar with that of the point-scale trends for all indices, the average trend magnitude showed an increase with the scale of the area on which precipitation was aggregated. Copyright (C) 2005 Royal Meteorological Society.
机译:在莱茵河盆地德国一侧,研究了1958年至2001年每日极端降水和温度的变化。在研究区域内的611个降水站和232个温度站上,计算了根据每日降水和温度的时间序列定义的一组极端降水和温度指数的趋势,并使用非参数Kendalltau检验检验了它们的对应意义。获得的结果表明,在研究期内,每日的最低和最高极端温度均有所增加,变化程度显示出季节性变化。从年度来看,发现每日最低极端温度的变化大于每日最高极端温度的变化。除夏季外,所有季节的每日极端强降水都显示出幅度和发生频率的增加趋势,夏季除外。日降水量的台站值也插值在5 km x 5 km的规则网格上,以便可以通过将插值的降水量聚合到任何所需的尺度来调查区域降水的指数变化。这使得能够评估极端降水变化的水文后果。尽管所有指数的空间格局都与点尺度趋势大致相同,但平均趋势幅度却显示出降水聚集区域的尺度增加。版权所有(C)2005皇家气象学会。

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