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Spatio-temporal precipitation changes and their localized predictors in the Taihang Mountain region, North China

机译:太空山区的时空降水变化及其本地化预测因子,华北地区

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摘要

Spatial-temporal variations in precipitation significantly influence infiltration, runoff, and other hydrological processes; and thus, in turn, they influence the risk of natural disasters such as flooding, drought, and erosion. Knowledge of these processes is still limited in the Taihang Mountain region, which is a highly heterogeneous environment in northern China. In this study, annual precipitation data for 1968-2017 from 88 weather stations in the Taihang Mountain region were analyzed. The Mann-Kendall (M-K) test and precipitation-related indices (precipitation amount, Sen's slope, Precipitation Concentration Index (PCI), and Coefficient of Variation (CV)) were used to analyze the spatial and temporal trends in precipitation in this region. Nine predictors (elevation, longitude, latitude, slope gradient, slope aspect, maximum temperature (Tmax), minimum temperature (Tmin), difference between Tmax and Tmin (DT), and evapotranspiration (ET)) were used to predict the precipitation and the related indices. The results reveal that the annual precipitation generally decreased from 1968 to 2017, but the M-K test indicates a nonsignificant trend. The precipitation decreased from southeast to northwest with significantly different spatial variations over the five decades investigated. The decrease in the PCI was not significant, and it generally decreased from northeast to southwest, suggesting a higher risk of flooding and drought in the northeast. The CV was 0.18-0.32, indicating a moderate spatial variation. In addition, the CV slightly decreased during the 50 years investigated. Multiple linear regression revealed that the amount of precipitation could be predicted from the latitude and longitude. The slope trend could be predicted based on latitude. PCI could be predicted based on longitude and elevation. CV could be predicted based on elevation, longitude, and Tmax. This suggests that the precipitation was mainly influenced by the geographical factors in the Taihang Mountain. This is useful information for the prediction of precipitation and for water management in this mountain region.
机译:降水的空间变化显着影响渗透,径流和其他水文过程;因此,反过来,它们影响了自然灾害的风险,如洪水,干旱和侵蚀。太空山区仍有限于中国北方的高度异质环境。在这项研究中,分析了太空山区88个气象站的1968 - 2017年的年降水数据。使用Mann-Kendall(M-K)测试和降水相关指数(降水量,森坡,析出浓度指数(PCI)和变异系数(CV))来分析该地区沉淀的空间和时间趋势。使用九个预测因子(高度,经度,纬度,斜率,斜坡方面,最大温度(Tmax),最小温度(Tmin),Tmax和Tmin(dt)之间的差异,以及蒸散蒸腾(et))来预测降水和相关索引。结果表明,年降水量普遍从1968年降至2017年,但M-K检验表明趋势不切实事。从东南到西北部的降水量随着调查的五十年而显着不同的空间变化。 PCI的减少并不显着,它通常从东北到西南部减少,暗示东北洪水和干旱的风险更高。 CV为0.18-0.32,表明中等空间变化。此外,在50年调查期间,CV略有下降。多元线性回归揭示了可以从纬度和经度预测降水量。可以基于纬度来预测坡度趋势。可以基于经度和高程来预测PCI。可以基于高程,经度和Tmax来预测CV。这表明降水主要受太空山区地理因素的影响。这是在该山区预测降水和水资源的有用信息。

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    Chinese Acad Sci Key Lab Agr Water Resources Hebei Lab Agr Water Saving Inst Genet & Dev Biol Hebei Key Lab Soil Ecol Ctr Agr Resources Res 286 Huaizhong Rd Shijiazhuang 050021 Hebei Peoples R China|Chinese Acad Sci Inst Subtrop Agr Key Lab Agro Ecol Proc Subtrop Reg Changsha 410125 Peoples R China;

    Chinese Acad Sci Key Lab Agr Water Resources Hebei Lab Agr Water Saving Inst Genet & Dev Biol Hebei Key Lab Soil Ecol Ctr Agr Resources Res 286 Huaizhong Rd Shijiazhuang 050021 Hebei Peoples R China;

    Chinese Acad Sci Key Lab Agr Water Resources Hebei Lab Agr Water Saving Inst Genet & Dev Biol Hebei Key Lab Soil Ecol Ctr Agr Resources Res 286 Huaizhong Rd Shijiazhuang 050021 Hebei Peoples R China|Univ Chinese Acad Sci Beijing 100049 Peoples R China;

    Chinese Acad Sci Key Lab Agr Water Resources Hebei Lab Agr Water Saving Inst Genet & Dev Biol Hebei Key Lab Soil Ecol Ctr Agr Resources Res 286 Huaizhong Rd Shijiazhuang 050021 Hebei Peoples R China;

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  • 正文语种 eng
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  • 关键词

    Taihang mountain; Rainfall variations; Mann-kendall test; Sen's slope; Precipitation concentration index; Geographical factors;

    机译:太空山;降雨变化;Mann-Kendall测试;森的坡度;降水浓度指数;地理因素;
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