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Spatiotemporal variation of long-term drought propensity through reliability-resilience-vulnerability based Drought Management Index

机译:通过可靠性 - 韧性 - 脆弱性的干旱管理指标的长期干旱倾向的时空变化

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This paper characterizes the long-term, spatiotemporal variation of drought propensity through a newly proposed, namely Drought Management Index (DMI), and explores its predictability in order to assess the future drought propensity and adapt drought management policies for a location. The DMI was developed using the reliability-resilience-vulnerability (RRV) rationale commonly used in water resources systems analysis, under the assumption that depletion of soil moisture across a vertical soil column is equivalent to the operation of a water supply reservoir, and that drought should be managed not simply using a measure of system reliability, but should also take into account the readiness of the system to bounce back from drought to a normal state. Considering India as a test bed, 5 year long monthly gridded (0.5 degrees Lat x 0.5 degrees Lon) soil moisture data are used to compute the RRV at each grid location falling within the study domain. The Permanent Wilting Point (PWP) is used as the threshold, indicative of transition into water stress. The association between resilience and vulnerability is then characterized through their joint probability distribution ascertained using Plackett copula models for four broad soil types across India. The joint cumulative distribution functions (CDF) of resilience and vulnerability form the basis for estimating the DMI as a five-yearly time series at each grid location assessed. The status of DMI over the past 50 years indicate that drought propensity is consistently low toward northern and north eastern parts of India but higher in the western part of peninsular India. Based on the observed past behavior of DMI series on a climatological time scale, a DMI prediction model comprising deterministic and stochastic components is developed. The predictability of DMI for a lead time of 5 years is found to vary across India, with a Pearson correlation coefficient between observed and predicted DMI above 0.6 over most of the study area, indicating a reasonably good potential for drought management in the medium term water resources planning horizon.Key Pointslist id="wrcr21136-list-0001" list-type="plain" list-item id="wrcr21136-li-0001"Drought Management Index (DMI) quantifies the drought propensity list-item id="wrcr21136-li-0002"Spatiotemporal variation of DMI helps in adapting management policies list-item id="wrcr21136-li-0003"Predictive potential of DMI can be used to assess the future drought propensity doi origin="wiley" registered="yes"10.1002/(ISSN)1944-7973/doi
机译:本文的表征通过新提出的即干旱管理指数(DMI)来表征了干旱倾销的长期时尚变化,并探讨了其可预测性,以评估未来的干旱倾向和适应地点的干旱管理政策。 DMI是使用常用于水资源系统分析中的可靠性 - 弹性 - 漏洞(RRV)理由的制定,假设垂直土壤柱的土壤水分消耗相当于供水水库的运行,并且干旱应该不仅仅使用系统可靠性的衡量标准,还应考虑到系统的准备情况从干旱到正常状态。将印度视为试床,每月5年长(0.5度LAT X 0.5度LON)土壤湿度数据用于计算在研究领域的每个网格位置的RRV。永久性衰弱点(PWP)用作阈值,指示转换为水胁迫。然后,通过使用Plackett Copula模型来表征弹性和脆弱性之间的关联,用于使用Plackett Copula模型进行印度的四种广泛的土壤类型。弹性和脆弱性的联合累积分配功能(CDF)构成了估算DMI作为评估每个网格位置的五年时间序列的基础。在过去的50年里,DMI的地位表明,在印度北部和北部和北部的印度北部和北部的北部和北部的北部和北部的北部,倾向于倾向,而且在半岛印度的西部持续。基于对DMI系列的过去行为在气候时间尺度上,开发了一种包括确定性和随机分量的DMI预测模型。发现5年的提前期DMI的可预测性在印度各种各样地发生,观察和预测DMI之间的Pearson相关系数超过0.6的大部分研究区域,表明在中期水中的干旱管理具有合理良好的潜力资源规划Horizo​​ n.key点<列表ID =“WRCR21136-LIST-0001”列表类型=“PLAIN”> 干旱管理指数(DMI)量化干旱倾向< List-Item ID =“WRCR21136-Li-Li-Li-0002”> DMI的时空变化在调整管理策略中有助于 DMI的预测潜力可用于评估未来的干旱倾向< Doi Origin =“Wiley”注册=“是”> 10.1002 /(ISSN)1944-7973

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