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首页> 外文期刊>Modern Applied Science >Regional Modeling of Climate Change Impacts on Groundwater Resources Sustainability in Peninsular Malaysia
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Regional Modeling of Climate Change Impacts on Groundwater Resources Sustainability in Peninsular Malaysia

机译:马来西亚半岛气候变化对地下水资源可持续性影响的区域模拟

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Projection of climate for the 2020s and 2080s from an ensemble of global climate models (GCMs) run under A2, A1B and B1 emission scenarios are used for regional modeling of climate change impacts on groundwater resources sustainability in Peninsular Malaysia. Few studies that have modeled climate change impacts on groundwater resources used the physically-based surface-subsurface flow model. In this paper, the suite of GCM outputs were modeled for the impact studies via integrative approach involving empirical modeling equation, GIS-based geostatistical technique and model forecasting accuracy optimization. A range of predictions is obtained by modeling the precipitation and temperature change factors derived from fifteen (15) GCMs forced with three (3) future emission scenarios for 50 years periods between 2000 to 2049 (2020s) and 2050 to 2099 (2080s) reference to the baseline period (1950 to 1999). The ensemble average suggests there will be a 1% reduction in monthly recharge in 2020s and 7-10% recharge increment in 2080s across the study area. The spread of predictions for recharge and PET rates across the area ranges from 12.05 to 17.83 mm/day and 3.72 to 4.05, respectively. Geostatistical analysis enabled generation of recharge rate and PET rate prediction maps. The prediction maps were classified into low (L), medium (M) and high (H) recharge and PET rated zones in GIS environment. The recharge rate model map revealed that more than 60% of the area coverage in the study area is characterized by low rating recharge, particularly within 2020s future period. The multiple climate models results provided the highest likelihood mean estimate as well as a measure of its uncertainty and less probable outcomes. Results suggest that recharge reduction in the area is an evidence of water resources scarcity in 2020s. The results of this work provided the basis for the inclusion of representative climate scenarios into the Peninsular Malaysia water resources’ existing decision support system model useful for policy and decision making in the area.
机译:根据在A2,A1B和B1排放情景下运行的一组全球气候模型(GCM)来预测2020年代和2080年代的气候,用于对马来西亚半岛的气候变化对地下水资源可持续性的影响进行区域建模。很少有模拟气候变化对地下水资源影响的研究使用基于物理的地表-地下流模型。在本文中,通过涉及经验建模方程,基于GIS的地统计技术和模型预测精度优化的综合方法,对用于影响研究的GCM输出套件进行了建模。通过对2000年至2049年(2020s)和2050年至2099年(2080s)之间的50年周期内由三(3)个未来排放情景强迫的十五(15)个GCM得出的降水和温度变化因子进行建模,可以获得一系列预测。基准期(1950年至1999年)。综合平均数表明,整个研究区域在2020年代的每月充电量将减少1%,在2080年代的充电量将增加7-10%。对该地区补给和PET费率的预测范围分别为12.05至17.83 mm /天和3.72至4.05。地统计分析可以生成补给率和PET率预测图。预测图分为GIS环境中的低(L),中(M)和高(H)补给以及PET额定区域。补给率模型图显示,研究区域超过60%的区域覆盖率具有较低的补给率,特别是在2020年代的未来时期。多种气候模型的结果提供了最高的均值估计值,以及其不确定性和可能性较小的度量。结果表明,该地区补给减少是2020年代水资源短缺的证据。这项工作的结果为将代表性的气候情景纳入马来西亚半岛水资源的现有决策支持系统模型提供了基础,该模型对于该地区的政策和决策很有用。

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