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首页> 外文期刊>Hydrological Processes >Impact of anticipated climate change on direct groundwater recharge in a humid tropical basin based on a simple conceptual model (pages 1655–1671)
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Impact of anticipated climate change on direct groundwater recharge in a humid tropical basin based on a simple conceptual model (pages 1655–1671)

机译:基于简单概念模型的预期气候变化对湿润热带盆地地下水直接补给的影响(第1655–1671页)

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摘要

A simple conceptual semi-distributed modelling approach for assessing the impacts of climate change on direct groundwaternrecharge in a humid tropical river basin is investigated. The study area is the Chaliyar river basin in the state of Kerala, India.nMany factors affecting future groundwater recharge include decrease or increase in precipitation and temperature regimes, coastalnflooding, urbanization and changes in land use. The model is based on the water-balance concept and links the atmospheric andnhydrogeologic parameters to different hydrologic processes. It estimates daily water-table fluctuation and is calibrated andnvalidated using 10 years of data. Data for the first 6 years (2000 to 2005) is used for model calibration, and data for the remainingnfour years (2006 to 2009) is used for validation. For assessing the impact of predicted climate change on groundwater rechargenduring the period 2071–2100, temperature and precipitation data in two post climate change scenarios, A2 and B2, werenpredicted using the Regional Climate Model (RCM), PRECIS (Providing Regional Climates for Impact Studies). These datanwere then corrected for biases and used in a hydrologic model to predict groundwater recharge in the post climate changenscenario. Due to lack of reliable data and proper knowledge as to the magnitude and extent of future climatic changes, it may notnbe possible to include all the possible effects quantitatively in groundwater recharge modelling. However, the study presents anscientific method to assess the impact of predicted climate change on groundwater recharge and would help engineers,nhydrologists, administrators and planners to devise strategies for the efficient use as well as conservation of freshwater resources.nCopyright © 2011 John Wiley & Sons, Ltd.
机译:研究了一种简单的概念性半分布式建模方法,用于评估气候变化对湿润热带流域地下水直接补给的影响。研究区域是印度喀拉拉邦的Chaliyar流域。n影响未来地下水补给的许多因素包括降水和温度状况的减少或增加,沿海洪水,城市化和土地利用的变化。该模型基于水平衡概念,并将大气和水文地质参数与不同的水文过程联系起来。它估计每日的地下水位波动,并使用10年的数据进行校准和验证。前6年(2000年至2005年)的数据用于模型校准,而其余4年(2006年至2009年)的数据用于验证。为了评估2071年至2100年期间预测的气候变化对地下水补给的影响,使用区域气候模型(RCM)PRECIS(为影响研究提供区域气候)预测了两个后气候变化情景A2和B2中的温度和降水数据。 )。然后对这些数据进行偏差校正,并在水文模型中用于预测气候变化后情景中的地下水补给。由于缺乏可靠的数据和对未来气候变化的幅度和程度的适当了解,可能无法在地下水补给模型中定量地包括所有可能的影响。但是,这项研究提出了一种评估预估的气候变化对地下水补给影响的科学方法,将有助于工程师,水文学家,管理人员和规划人员制定有效利用和保护淡水资源的策略。n版权所有©2011 John Wiley&Sons ,Ltd.

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