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首页> 外文期刊>Advances in Meteorology >Spatial and Temporal Variability of Precipitation in Haihe River Basin, China: Characterization and Management Implications
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Spatial and Temporal Variability of Precipitation in Haihe River Basin, China: Characterization and Management Implications

机译:中国海河流域降水的时空变化:特征与管理意义

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摘要

Data analysis and characterization of precipitation in the Haihe River Basin (HRB) of China are required for management practices for the purpose of flood water control and utilization. In the companion paper, we presented precipitation data in the HRB during 1951–2010 and reported its basic statistics such as temporal trend and spatial variability. In this study, spatiotemporal variability on the precipitation was further investigated comprehensively for the underlying physics and the implication to water resource management. During the summer flood season of the study area, basin-wide precipitation was negatively correlated to average NINO3.4 index. Spatially, summer precipitation was correlated with gridded sea surface temperature (SST) observed in the eastern tropic Pacific Ocean and the western tropic Indian Ocean. SST in two representative areas was identified as potential predictors for precipitation in the HRB. No spatial or temporal correlations were confirmed between precipitation and soil moisture as annual averages in the study area. Copula analysis suggested about 40% possibility in a year with a potential for cross-watershed water diversion within HRB.
机译:为了控制和利用洪水,管理实践需要对中国海河流域(HRB)的降水资料进行数据分析和特征分析。在随附的论文中,我们介绍了1951-2010年高铁基地的降水数据,并报告了其基本统计数据,例如时间趋势和空间变异性。在这项研究中,对降水的时空变化进行了进一步的综合研究,以了解基础物理及其对水资源管理的影响。在研究区域的夏季汛期,流域范围内的降水与NINO3.4平均值呈负相关。在空间上,夏季降水与东热带太平洋和西热带印度洋中观测到的网格海面温度(SST)相关。在两个代表性地区的SST被确定为HRB降水的潜在预测因子。研究区域的年平均降水量与土壤湿度之间没有空间或时间相关性。 Copula分析表明,一年之内约有40%的可能性在HRB内进行跨集水区的引水。

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