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滨江流域降水时空演变规律分析

ISSN号：1000-0852
期刊名称：《水文》
时间：0
分类：P468.24[天文地球—大气科学及气象学]
作者机构：[1]中山大学水资源与环境研究中心,广东广州510275, [2]华南地区水循环和水安全广东普通高校重点实验室,广东广州510275, [3]水利部珠江水利委员会珠江水利综合技术中心,广东广州510610
相关基金：国家自然科学基金重大国际合作和重点项目（51210013,50839005）;国家科技支撑计划（2012BAC2180103）;水利部公益项目（201201094,201301002-02）;广东省科技厅项目（20108050300010）;广东省水利科技创新项目（2011-11,2009-39）;中英瑞气候变化适应项目广东气候变化风险评估及适应对策研究（ACCC/20100705-11

作者：丁华龙, 肖卫国[3], 陈晓宏[1,2], 张云[1,2], 陈玲玲[1,2]

关键词：降水量, Mann—Kendall, Mann—Whitney—Pettitt, 时空演变, 变异, 滨江流域, precipitation, Mann-Kendall, Mann-Whitney-Pettitt, temporal-spatial evolution, variation, Binjiang River Basin

中文摘要：

降水是水循环的关键环节,直接影响着径流过程和可利用水资源量的时空分布,关系到区域水资源安全和可持续发展.为了探讨气候变化下华南湿润区典型小流域降水时空演变规律,利用珠江流域北江一级支流滨江流域内及其邻近共10个站点近47年日降水量观测资料,采用非参数统计方法Mann-Kendall（M-K）趋势检验和Mann-Whitney-Pettiu （MWP）检定方法,对年、汛期/非汛期、年日最大和年月最大降水量进行分析.结果表明：滨江流域多年平均降水量呈北少南多分布,主要与区域气流走向及流域地形有关;年降水量总体呈现减少趋势,其中流域南部呈显著减少趋势,北部呈不显著减少趋势,其主要是汛期（4～9月）降水量减少,非汛期（10～翌年3月）降水量变化不大;年日最大和年月最大降水量均呈减少趋势.流域南部年降水量和汛期降水量在1983年发生了显著性变异;流域北部年最大日降水量和年月最大降水量分别在1987年和1985年左右发生显著性变异.

英文摘要：

The precipitation is the key process in water cycle. It directly affects temporal and spatial distribution of runoff process and amount of available water resources. To investigate space-time evolution of precipitation in typical small watersheds of southern China under climate change, this paper analyzed the annual precipitation, flood season and non-flood season precipitation, annual maximum daily precipitation and annual maximum monthly precipitation by using the nonparametrie statistics including Mann Kendall trend test method and Mann-Whitney- Pettitt verification method based on the 47-year observed daily precipitation from 10 stations in the Binjiang River Basin, a tributary of the Beijiang River in the Pearl River Basin. The result shows that the multi-year average precipitation of the northern part in the basin is less than that in the south, which has close relation to regional airflow direction and valley terrain. At the same time, general decline of annual precipita- tion, including southern basin has a significant decline and the northern part shows no significant decline, which is mainly the precipitation in the flood season （April-September） reduced, while the precipitation in non-flood season （October-March in the next year） changed little. Both annual maximum daily precipitation and annual maximum monthly precipitation have a trend of decrease. The annual precipitation and flood season precipitation in the southern part of the basin had a significant variation in 1983, while in the north, the annual maximum daily precipi- tation and annual maximum monthly precipitation have respectively significant variation in 1987 and 1985.

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