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首页> 外文期刊>Hydrological ProcHydrological Processesrnesses >Spatial and temporal variability of precipitation extrema in the Haihe River Basin, China
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Spatial and temporal variability of precipitation extrema in the Haihe River Basin, China

机译:海河流域降水极值的时空变异。

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摘要

In this article, we investigated the variability of precipitation conditions in the Haihe River basin (HRB) during 1961–2010 by analyzing four daily precipitation scenarios. These scenarios were set with the values of, equal to 0 mm/day, 10–20 mm/day, 20–50 mm/day, and greater than 50 mm/day, which were denoted as P0, P10, P20, and P50, respectively. Results indicate that the mean values of daily precipitation decline, and its fluctuation becomes weak with years in HRB. The contour of daily precipitation with the mean value of 1.4 mm/day moves more than 100 km toward southeast in the basin from 1960s to 2000s. The variations of four precipitation scenarios show difference. The Tianjin and Langfang cities were the P0 drought center in HRB after 1980s, and the days and regions without precipitation increase with years. The magnitude of P10 extrema shows no significant changes over the last 50 years, but the rainfall centers vary with areas in HRB. The magnitude of P20 extrema shows no obvious changes in 1961–2000 but increases in 2000s. The magnitude of P50 extrema obviously declines in the last 50 years, with the rainfall center moving from northeast to south of HRB. Urbanization impacts are reflected in some cities in 1980s and 1990s, but after 2000, the urbanization impacts were not clearly detected due to the significant precipitation decreases in HRB. In summary, precipitation decrease is caused by the decreases of P50 extrema rather than P10 and P20 extrema in HRB, which would be favorable for the flood resources utilization through ample-low flow operations over space. Copyright © 2012 John Wiley & Sons, Ltd.
机译:在本文中,我们通过分析四种日常降水情景,调查了1961-2010年海河流域(HRB)降水条件的变化。这些方案的设置值分别为0毫米/天,10-20毫米/天,20-50毫米/天以及大于50毫米/天,分别表示为P0,P10,P20和P50 , 分别。结果表明,HRB中,年降水量的平均值下降,并且其波动随着年份而变弱。从1960年代到2000年代,日平均降水量为1.4毫米/天的轮廓向盆地东南方向移动了100多公里。四种降水情景的变化表现出差异。天津市和廊坊市是1980年代后HRB的P0干旱中心,无降水的日子和地区随年增加。在过去的50年中,P10极端值的变化没有显着变化,但是降雨中心随HRB地区的变化而变化。 P20极值的大小在1961–2000年没有明显变化,但在2000年代有所增加。在过去的50年中,P50极值的幅度明显下降,降雨中心从HRB的东北向南移动。在1980年代和1990年代,一些城市反映了城市化的影响,但是在2000年之后,由于HRB降水量的显着减少,并未明确发现城市化的影响。综上所述,降水减少是HRB的P50极值而不是P10和P20极值的减少所致,这将有利于通过空间内的低流量充分利用洪水资源。版权所有©2012 John Wiley&Sons,Ltd.

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    Institute of Geographic Sciences and Natural Resources Research Chinese Academy of Sciences Key Laboratory of Water Cycle Related Land Surface Processes Beijing China. Chinese Academy of Sciences Center for Water Resources Research Beijing China;

    Institute of Geographic Sciences and Natural Resources Research Chinese Academy of Sciences Key Laboratory of Water Cycle Related Land Surface Processes Beijing China. Chinese Academy of Sciences Center for Water Resources Research Beijing China;

    Institute of Geographic Sciences and Natural Resources Research Chinese Academy of Sciences Key Laboratory of Water Cycle Related Land Surface Processes Beijing China. Chinese Academy of Sciences Center for Water Resources Research Beijing China;

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  • 正文语种 eng
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  • 关键词

    precipitation; precipitation extrema; climate change; urbanization; drought; Haihe River Basin;

    机译:降水;降水极端;气候变化;城市化;干旱;海河流域;

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