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Regional analysis of streamflow drought: a case study in southwestern Iran

机译:径流干旱的区域分析:以伊朗西南部为例

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摘要

Droughts are complex natural hazards that, to a varying degree, affect some parts of the world every year. The range of drought impacts is related to drought occurring in different stages of the hydrological cycle and usually different types of droughts such as meteorological, agricultural, hydrological, and socio-economical are the most distinguished types. Hydrological drought includes streamflow and groundwater droughts. In this paper, streamflow drought was analyzed using the method of truncation level (at 70 % level) by daily discharges at 54 stations in southwestern Iran. Frequency analysis was carried out for annual maximum series of drought deficit volume and duration. 35 factors such as physiographic, climatic, geologic and vegetation were studied to carry out the regional analysis. According to conclusions of factor analysis, the six most effective factors include watershed area, the sum rain from December to February, the percentage of area with NDVI <0.1, the percentage of convex area, drainage density and the minimum of watershed elevation, explained 89.2 % of variance. The homogenous regions were determined by cluster analysis and discriminate function analysis. The suitable multivariate regression models were ascertained and evaluated for hydrological drought deficit volume with 2 years return period. The significance level of models was 0.01. The conclusion showed that the watershed area is the most effective factor that has a high correlation with drought deficit volume. Moreover, drought duration was not a suitable index for regional analysis.
机译:干旱是复杂的自然灾害,每年都会在不同程度上影响世界某些地区。干旱影响的范围与在水文循环不同阶段发生的干旱有关,通常最不同类型的干旱是气象,农业,水文和社会经济干旱。水文干旱包括径流和地下水干旱。本文采用截断水平法(在70%的水平)通过伊朗西南部54个站的日排放量分析了径流干旱。进行了频率年度干旱亏缺量和持续时间的最大系列的频率分析。研究了地貌,气候,地质和植被等35个因素,进行了区域分析。根据因子分析的结论,最有效的六个因子包括流域面积,12月至2月的总降雨量,NDVI <0.1的面积百分比,凸面面积的百分比,排水密度和流域最低海拔,解释为89.2。差异百分比。通过聚类分析和区分功能分析确定同质区域。确定了合适的多元回归模型,并评估了回归期为2年的水文干旱赤字量。模型的显着性水平为0.01。结论表明,流域面积是与干旱亏缺量高度相关的最有效因素。此外,干旱持续时间不是进行区域分析的合适指标。

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