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United Kingdom daily precipitation intensity: improved early data, error estimates and an update from 2000 to 2006

机译:英国每日降水强度:改进的早期数据,误差估计以及2000年至2006年的更新

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This paper updates the analysis by Osborn et al. of trends in the contribution of heavy events to precipitation in the UK. We spatially extended the previous analysis of 110 rain gauges to a set of 689 rain gauges covering almost the whole UK, and updated the results to November 2006. For each station and season, we calculated ten time series of the contribution of ten precipitation amount categories to the total seasonal precipitation. A principal component analysis of post-1961 trends of all categories and stations is consistent with earlier results, namely, widespread shifts towards greater contribution from heavier precipitation categories during winter, and towards light and moderate categories during summer. Regional and UK average time series of the contribution from the category consisting of the heaviest events indicate that the increased winter intensity was sustained during the most recent ten years, but the trend did not continue at the rate reported previously for 1961-1995. For summer, the decreasing contribution from the heaviest rainfall category reported for 1961-1995 underwent a reversal during the most recent decade, returning towards the 1961-1995 reference level of intensity. Confidence intervals for these regional and UK average time series were estimated by a bootstrap approach and indicate that the sparser observations from the first half of the 20th century are still sufficient to estimate UK average change. These longer records support the existence of a long-term increase in winter precipitation intensity, and similar trends have now also become evident in spring and (to a lesser extent) autumn. The summer rainfall intensity has exhibited changes that are more consistent with inter-decadal variability than any overall trend. Copyright (c) 2008 Royal Meteorological Society.
机译:本文更新了Osborn等人的分析。英国大事件对降水的贡献趋势。我们将先前对110个雨量计的分析在空间上扩展到了覆盖整个英国的689个雨量计,并将结果更新至2006年11月。对于每个气象站和每个季节,我们计算了十个降水量类别贡献的十个时间序列总季节降水量。 1961年后所有类别和站点趋势的主成分分析与早期结果一致,即,广泛的变化趋势是冬季较重的降水类别向更大的贡献,而夏季则向轻度和中等类别转变。地区和英国平均时间序列从最重的事件组成的类别中得出的贡献表明,冬季强度的增加在最近十年中得以维持,但这种趋势并没有以先前报告的1961-1995年的速率持续。在夏季,最近十年中,1961-1995年降雨量最大的类别的贡献下降,但在最近十年中出现了逆转,回到了1961-1995年强度参考水平。这些区域和英国平均时间序列的置信区间是通过自举法估算的,表明从20世纪上半叶的稀疏观测仍然足以估算英国的平均变化。这些较长的记录支持冬季降水强度长期增加的存在,并且类似的趋势现在在春季和(在较小程度上)秋季也变得明显。夏季降雨强度的变化与年代际变化相比,比任何总体趋势都更为一致。版权所有(c)2008皇家气象学会。

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