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Climatological features and trends of extreme precipitation during 1979-2012 in Beijing, China

机译:1979-2012年中国北京的极端降水气候特征和趋势

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In this study, three kinds of hourly precipitation series with the spatial resolution of 0.1° are used to analyze the climatological features and trends of extreme precipitation during the period of 1979-2012 in Beijing, China. The results show that: (1) the spatial distribution of median annual precipitation, with a range from 500 to 825 mm, is similar to that of local topography, which increases from the northwest to the southeast. Taking the urban area as a centre, the inter-annual precipitation in the Beijing area displays an outward decreasing tendency at the maximum rate of 125 mm per decade (125 mm × 10 a~(-1)); (2) extreme precipitation amount, which accounts for 40-48 % of total precipitation amount, has a similar spatial distribution to average annual precipitation; (3) the spatial distribution of extreme precipitation days and threshold estimated as the upper 95 percentile are significantly different from that of extreme precipitation, with maximum values concentrated on the urban area and the eastern mountain area, and minimum values in northwest; (4) extreme precipitation days (Ex_pd95) show an opposite distribution to extreme precipitation threshold (Ex_pv95), indicating that areas with greater precipitation threshold may has less precipitation days, and vice versa; (5) an apparent spatiotemporal decreasing tendency is detected in extreme precipitation amount. The downward tendencies are also found in extreme precipitation threshold. Unlike Ex_pv95, in most of the study area, Ex_pd95 is virtually unchanged; (6) downward trends of extreme precipitation is slightly smaller than that of annual precipitation, and the reducing amplitude of north-eastern areas are much higher than the areas in the southwest.
机译:本文利用空间分辨率为0.1°的三种小时降水序列分析了1979-2012年北京地区极端降水的气候特征和变化趋势。结果表明:(1)年平均降水量的空间分布在500mm至825mm之间,与局部地形相似,从西北向东南逐渐增加。以市区为中心,北京地区的年际降水呈现出逐年减少的趋势,最大速率为125 mm / 10s(125 mm×10 a〜(-1))。 (2)极端降水量占总降水量的40-48%,其空间分布与年均降水量相似; (3)极端降水日的空间分布和估计的阈值(最高95个百分位数)与极端降水的空间分布有显着差异,最大值集中在市区和东部山区,而最小值集中在西北地区; (4)极端降水日数(Ex_pd95)与极端降水阈值(Ex_pv95)的分布相反,表明具有较高降水量阈值的区域可能具有较少的降水日数,反之亦然; (5)极端降水量存在明显的时空下降趋势。在极端降水阈值中也发现了下降趋势。与Ex_pv95不同,在大多数研究领域中,Ex_pd95几乎没有变化。 (6)极端降水的下降趋势略小于年降水量的下降趋势,东北地区的下降幅度远高于西南地区。

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