中国杭州百年降水和极端降水的气候特征

Kuo Wang, Han Zhang, Mengying Bao, Zhengquan Li, Gaofeng Fan
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摘要

本研究利用杭州基站的气象观测资料,分析了全球气候变化背景下浙江省杭州市的降水特征。我们从百年趋势、季节变化、周期性和极端降水变化等几个方面研究了杭州降水的气候特征。研究结果表明,杭州市降水量在百年尺度上呈线性递减趋势,并具有明显的年代际特征。进入 21 世纪以来,降水波动幅度明显增大。在百年尺度上的季节降水量年代际变化中,秋季降水量呈 8.1 mm/10a 的递减趋势,而其他三个季节的递减趋势在统计上不显著。在过去 30 年中,杭州春季降水呈减少趋势,冬季呈增加趋势。我们的分析揭示了明显的降水周期,包括 20 世纪 60 年代以来的准 30 年周期和 20 世纪 80 年代以来的准 10 年周期。然而,在过去 10 年中,这种周期性有所减弱。此外,暴雨发生率在过去 10 年迅速增加。此外,受全球气候变化和区域过程的影响,杭州市极端降水量的变化与年降水量的总体趋势有较强的相关性。1951-1980年杭州市年最大日降水量主要在0-40毫米之间,1981-2010年主要在40-80毫米之间,最大日降水量出现率分别为1.41次/10a和1.89次/10a。该研究强调了短时强降雨引发城市内涝的风险,为杭州市极端气象水文灾害风险评估提供了有益参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Climatic characteristics of centennial and extreme precipitation in Hangzhou, China
The precipitation characteristics in Hangzhou of Zhejiang Province, China under the background of global climate change are analyzed using the meteorological observation data obtained from the Hangzhou base station in this study. We investigate the climate characteristics of precipitation in Hangzhou from several aspects, such as centennial trend, seasonal change, periodicity and the variation of extreme precipitation. Our results show a linear decreasing trend and obvious interdecadal characteristics in the precipitation of Hangzhou on a centennial timescale. Significantly increased amplitude of precipitation fluctuation was observed since the beginning of the 21st century. For the interdecadal variation of seasonal precipitation on a centennial timescale, precipitation in autumn showed a decreasing trend of 8.1 mm/10a, whereas the trends for the other three seasons were statistically insignificant. The precipitation in Hangzhou showed a decreasing trend in spring and an increasing trend in winter over the past 30 years. Our analyses reveal distinct precipitation cycles, including a quasi-30-year cycle since the 1960s and a quasi-10-year cycle since the 1980s. However, the periodicity has weakened in the past 10 years. In addition, the occurrence of torrential rain has increased rapidly in the past 10 years. Furthermore, influenced by global climate change and regional processes, the variation of extreme precipitation in Hangzhou has changed, which shows strong correlations with the overall trend of annual precipitation. The annual maximum daily precipitation in Hangzhou was mainly in the range of 0-40 mm from 1951 to 1980 and in the range of 40-80 mm from 1981 to 2010 with the maximum daily precipitation occurrence rate of 1.41 times/10a and 1.89 times/10a, respectively. This study emphasizes the risk of urban waterlogging caused by short-term heavy rainfall and provides useful reference to the assessment of extreme meteorological and hydrological disaster risk in Hangzhou.
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