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Characterization of Regional Drought Over Water and Energy Limited Zones of India Using Potential and Actual Evapotranspiration

机译:利用潜力和实际蒸散对印度水和能量有限区的区域干旱的特征

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Understanding the drought characteristics is critical for water resources management in water stressed countries such as India. Previous studies evaluating drought assessments over India considered precipitation (P) and potential evapotranspiration (PET) as drivers using standardized precipitation‐evapotranspiration index (SPEI). The suitability of actual evapotranspiration (AET), which accounts for both water and energy based evaporative demands, in drought characterization is limited. In this study, SPEI is restructured with AET to characterize the regional drought over water and energy limited regions as standardized precipitation actual evapotranspiration index (SPAEI). For this, AET estimated based on Budyko framework and remote sensing‐based AET data has been used. The original formulation of SPEI is limited toward capturing the seasonality present in P and PET. The SPEI is restructured to account for the water availability deficit in the drought assessment rather than the actual atmospheric water demand in a given period to capture the strong seasonality of rainfall. The study compared the drought characteristics with both PET and AET for various meteorological homogeneous zones of India, which are characterized as water‐limited (Central, North, West, South, and Jammu and Kashmir, J&K) and energy‐limited (Northeast and Northeast hills) zones. Overall, the proposed new drought index based on AET can be promising toward drought intensity, extreme drought areal extents, shorter‐time scale drought frequencies, and longer‐time scale drought durations for water‐limited zones. The proposed drought indices based on AET can be robust for the drought assessment under consideration of water energy along with land and vegetation variability and can provide more insights for water‐limited regions.
机译:了解干旱特征对于印度等水资源管理的水资源管理至关重要。以前的研究通过使用标准化沉淀蒸发指数(SPEI)评估印度的干旱评估被认为是沉淀(P)和潜在的蒸发剂(PET)作为司机。实际蒸散(AET)的适用性,其在干旱表征中考虑了水和能量的蒸发需求,是有限的。在这项研究中,Spei与AET重组,以表征水和能量限量区域的区域干旱,作为标准化降水实际蒸发散料指数(SPAEI)。为此,已经使用了基于Budyko框架和基于遥感的AET数据的AET。 Spei的原始配方仅限于捕获P和PET中存在的季节性。 Spei被重组,以解释干旱评估中的水可用性赤字,而不是在特定时期内的实际大气水需求,以捕捉到暴雨的强烈季节性。该研究将宠物和AET与印度各种气象均地区的干旱特性进行了比较,其被称为水有限公司(中央,北,西,南,南,Jammu和Kashmir,J&K)和能源有限公司(东北和东北山丘)区域。总体而言,基于AET的拟议的新干旱指数可能对干旱强度,极端干旱的面积,较短时间的干旱频率,以及用于有限区域的较短时间尺度干旱持续时间。基于AET的拟议的干旱指数对于在考虑水能以及土地和植被变异性的情况下对干旱评估具有稳健,并且可以为有限的地区提供更多的见解。

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