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Assessment of climate change impacts on drought severity using SPI and SDI over the Lower Nam Phong River Basin, Thailand

机译:利用SPI和SDI在泰国下游南部南部的南部和SDI对干旱严重程度的评估

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The Lower Nam Phong River Basin, which is located in Northeast Thailand, is impacted by drought, which is likely to increase in severity in the future. Since drought seriously affects human life and well-being, this assessment was focused on the impacts of climate change on drought severity in the Lower Nam Phong River Basin. Daily climate data, such as rainfall and temperatures, for 2020 to 2050 under emission scenario Representative Concentration Pathway (RCP8.5), were obtained from “HadGEM2-AO”, downscaled by the Regional Climate Model version 4 (RegCM4), and bias-corrected via the Delta Change Method. Drought conditions were then classified based on the Standardized Precipitation Index (SPI) calculated from future daily rainfall, and the Streamflow Drought Index (SDI) derived from future daily discharge at each sub-basin outlet obtained from the Soil and Water Assessment Tool (SWAT) model simulations. At the E.22B gauging station, the SWAT performance was found to be satisfactory for all evaluation criteria, i.e. R2 and NSE values were 0.86 and 0.74 for calibration (2005 – 2010), and 0.92 and 0.89 for validation (2011 – 2016), respectively. For drought risk assessment, the point-based SPI and SDI values at 3- and 6-month time scales were spatially interpolated using kriging to assess short-term drought conditions. Based on the SPI-6 during the mid-future period (2041 – 2050), the Lower Nam Phong River Basin would have the highest chance of drought with cumulative frequency of 90.7%, whereas based on SDI-6 the highest chance of drought would occur during the near-future period (2031 – 2040) with cumulative frequency of 97.5%. These findings imply that both SPI and SDI indices can be used as good alternatives for monitoring droughts in the Lower Nam Phong River Basin; however, validation is required to ensure forecast accuracy of droughts in the near- to mid-future time horizons.
机译:位于泰国东北部的下部南部Phong River盆地受干旱影响,这可能会在未来严重程度增加。由于干旱严重影响人的生命和福祉,因此该评估专注于气候变化对下纳姆Phong河流域干旱严重程度的影响。每日气候数据,如降雨和温度,为2020年至2050年在发射方案代表浓度途径(RCP8.5)下,由“Hadgem2-AO”获得,由区域气候模型4(REGCM4)缩小,和偏见 - 通过Delta Change方法校正。然后根据从未来日落降雨计算的标准化降水指数(SPI)分类干旱条件,以及从土壤和水评估工具(SWAT)中的每个副盆地出口的未来日出的流水流干旱指数(SDI)模型模拟。在E.22B测量站​​,发现SWAT性能对于所有评估标准,IE R2和NSE值为0.86和0.74,用于验证(2005 - 2010)和0.92和0.89(2011年 - 2016),分别。对于干旱风险评估,使用Kriging来评估短期干旱条件,在空间内插的基于点的SPI和SDI值。基于SPI-6期间的中期期间(2041 - 2050),下纳姆Phong River河流域的累积频率最高的机会为90.7%,而基于SDI-6最高的干旱机会在近期期间(2031-2040)在累计频率为97.5%时发生。这些发现意味着SPI和SDI指数都可以用作监测下部Nam Phong River流域的良好替代品;但是,需要验证以确保在未来的中期时间视野中预测干旱的准确性。

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