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Simulation of meteorological drought using exponential smoothing models: a study on Bankura District, West Bengal, India

机译:使用指数平滑模型模拟气象干旱:印度西孟加拉邦班库拉地区的研究

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Water scarcity and drought management is the burning issue in India and hence needs serious attention of researchersto develop rigorous plan and management. Areas that belong to various plateaus, e.g., Chotanagpur plateau, Deccanplateau, etc., are mostly affected by drought in India. In the past decade, Bankura District of West Bengal, which belongsto northeast part of Chotanagpur plateau, faced severe drought several times. However, the assessment of droughtscenario in this area is far from conclusive statement till date. In this paper, we simulate standardized precipitation index(SPI) using double exponential (DE) and Holt–Winter exponential smoothing model (HW) for several time steps (e.g.,3 months, 6 months, 12 months, 24 months and 48 months) in the time period of 1979–2014. The comparative analysisbetween two models indicates that DE is more accurate one. DE is observed with relatively low root mean squared error(RMSE) and high R~2 value. Furthermore, drought-prone zones are demarcated using combined scores of principal componentanalysis (PCA) and those combined scores are estimated using actual, HW and DE simulated SPI in several timesteps. At the shorter (3 and 6 months) and longer time step (12, 24 and 48 months), the PCA demonstrates almost sameresults. The western and northwestern blocks of the district are severely affected by drought, and the southern portionsare at mild condition. Spatially distributed RMSE in every time steps is also high in northwestern portions of the studyregion. Our result may be useful to understand the pattern of drought to take necessary action in management of waterresources in Bankura District, West Bengal. Moreover, the study uses an unique methodology to simulate and assessmeteorological drought, which is applicable in any region of the world.
机译:缺水和干旱管理是印度亟待解决的问题,因此需要研究人员认真关注制定严格的计划和管理。属于各个高原的区域,例如Chotanagpur高原,Deccan高原等受印度干旱的影响最大。在过去的十年中,西孟加拉邦的班库拉区在Chotanagpur高原的东北部,几次遭受严重干旱。但是,干旱评估迄今为止,该领域的情景还没有定论。在本文中,我们模拟标准化降水指数(SPI)使用双重指数(DE)和Holt-Winter指数平滑模型(HW)进行多个时间步长(例如,1979-2014年的3个月,6个月,12个月,24个月和48个月)。比较分析在两个模型之间表示DE更准确。观察到DE的均方根误差相对较低(RMSE)和较高的R〜2值。此外,利用主要成分的综合得分划定干旱多发区分析(PCA)和这些综合得分是使用实际,硬件和DE模拟SPI多次估算的脚步。在较短的时间(3和6个月)和较长的时间(12、24和48个月)中,PCA表现出几乎相同的结果结果。该地区的西部和西北地区受到干旱的严重影响,而南部地区处于温和状态。在研究的西北部,每个时间步的空间分布RMSE也很高地区。我们的结果可能有助于了解干旱的模式,以便在水管理方面采取必要的行动西孟加拉邦Bankura区的资源。此外,这项研究使用了独特的方法来模拟和评估气象干旱,适用于世界任何地区。

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