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Mapping groundwater resiliency under climate change scenarios: A case study of Kathmandu Valley, Nepal

机译:气候变化情景下的地下水弹性:尼泊尔加德满都谷的案例研究

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摘要

Groundwater resources of Kathmandu Valley in Nepal are under immense pressure from multiple stresses, including climate change. Due to over-extraction, groundwater resources are depleting, leading to social, environmental and economic problems. Climate change might add additional pressure by altering groundwater recharge rates and availability of groundwater. Mapping groundwater resilience to climate change can aid in understanding the dynamics of groundwater systems, facilitating the development of strategies for sustainable groundwater management. Therefore, this study aims to analyse the impact of climate change on groundwater resources and mapping the groundwater resiliency of Kathmandu Valley under different climate change scenarios. The future climate projected using the climate data of RCM's namely ACCESS-CSIRO-CCAM, CNRM-CM5-CSIRO-CCAM and MPI-ESM-LR-CSIRO-CCAM for three future periods: near future (2010-2039), mid future (2040-2069) and far future (2070-2099) under RCP 4.5 and RCP 8.5 scenarios were bias corrected and fed into the Soil and Water Assessment Tool (SWAT), a hydrological model, to estimate future groundwater recharge. The results showed a decrease in groundwater recharge in future ranging from 3.3 to 50.7 mm/yr under RCP 4.5 and 19-102.1 mm/yr under RCP 8.5 scenario. The GMS-MODFLOW model was employed to estimate the future groundwater level of Kathmandu Valley. The model revealed that the groundwater level is expected to decrease in future. Based on the results, a groundwater resiliency map of Kathmandu Valley was developed. The results suggest that groundwater in the northern and southern area of the valley are highly resilient to climate change compared to the central area. The results will be very useful in the formulation and implementation of adaptation strategies to offset the negative impacts of climate change on the groundwater resources of Kathmandu Valley.
机译:尼泊尔加德满都山谷的地下水资源受到多重压力的巨大压力,包括气候变化。由于过度提取,地下水资源耗费,导致社会,环境和经济问题。通过改变地下水补给率和地下水的可用性,气候变化可能会增加额外的压力。地下水适应气候变化可以帮助理解地下水系统的动态,促进了可持续地下水管理的战略。因此,本研究旨在分析气候变化对地下水资源的影响,并在不同气候变化方案下绘制加德满都谷的地下水弹性。未来的气候,使用RCM的气候数据,即进入CSIRO-CCAM,CNRM-CM5-CSIRO-CCAM和MPI-ESM-LR-CSIRO-CCAM的三个未来期间:不久的将来(2010-2039),中期未来( 2040-2069)和遥远的未来(2070-2099)在RCP 4.5和RCP 8.5方案中偏离校正并喂入土壤和水分评估工具(SWAT),水文模型,估算未来的地下水补给。结果表明,在RCP 8.5场景下,未来在RCP 4.5和19-102.1mm / yr下的3.3至50.7 mm / yr的下降率降低。 GMS-Modflow模型用于估计加德满都谷的未来地下水位。该模型透露,预计地下水位将来会降低。基于结果,开发了加德满都谷的地下水弹性图。结果表明,与中心地区相比,山谷北部和南部地区的地下水对气候变化非常有弹性。结果在制定和实施适应策略方面非常有用,以抵消气候变化对加德满都山谷地下水资源的负面影响。

著录项

  • 来源
    《Environmental research》 |2020年第4期|109149.1-109149.14|共14页
  • 作者单位

    Water Engineering and Management School of Engineering and Technology Asian Institute of Technology P.O. Box 4 Klong Luang Pathum Thani 12120 Thailand;

    Water Engineering and Management School of Engineering and Technology Asian Institute of Technology P.O. Box 4 Klong Luang Pathum Thani 12120 Thailand;

    Water Engineering and Management School of Engineering and Technology Asian Institute of Technology P.O. Box 4 Klong Luang Pathum Thani 12120 Thailand;

    International Water Management Institute (IWMI) Nepal Office Shree Durbar Pulchowk Lalitpur 3 GPO Box 8975 EPC 416 Kathmandu Nepal;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Climate change; GMS-MODFLOW; Groundwater resiliency; Kathmandu valley; RCP;

    机译:气候变化;gms-modflow;地下水弹性;加德满都山谷;rcp.;

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