Abstract

PurposeGroundwater is an important source of water supply in arid and semi-arid areas. The purpose of this study is to predict the impact of climate change on groundwater recharge in an arid environment in Ilam Province, west of Iran.Design/methodology/approachA three-dimensional transient groundwater flow model (modular finite difference groundwater FLOW model: MODFLOW) was used to simulate the impacts of three climate scenarios (i.e. an average of a long-term rainfall, predicted rainfall in 2015-2030 and three years moving average rainfall) on groundwater recharge and groundwater levels. Various climate scenarios in Long Ashton Research Station Weather Generator were applied to predict weather data.FindingsHadCM3 climatic model and A2 emission scenario were selected as the best methods for weather data generation. Based on the results of these models, annual precipitation will decrease by 3 per cent during 2015-2030. For three emission scenarios, i.e. an average of a long-term rainfall, predicted rainfall in 2015-2030 and three years moving average rainfall, precipitation in 2030 is estimated to be 265, 257 and 247 mm, respectively. For the studied aquifer, predicted recharge will decrease compared to recharge calculated based on the average of long-term rainfall.Originality/valueThe decline of groundwater level in the study area was 11.45 m during the past 24 years or 0.48 m/year. Annual groundwater depletion should increase to 0.75 m in the coming 16 years via climate change. Climate change adaptation policies in the basin should include changing the crop type, as well as water productivity and irrigation efficiency enhancement at the farm and regional scales.

Highlights

  • An increase in the average ocean level, air temperatures, general melting of ice, sea level and many other factors leads to climate warming (IPCC, 2007)

  • The main aim of this study is to evaluate how climate change should change groundwater recharge in the coming decades

  • HADCM3 was selected as the best model for Mosian basin (R2 = 74 per cent)

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Summary

Introduction

An increase in the average ocean level, air temperatures, general melting of ice, sea level and many other factors leads to climate warming (IPCC, 2007). These predictions indicate that water resources would be affected by climate change (IPCC, 2008), which in turn affect the components of water cycle such as precipitation, evaporation and evapotranspiration and International Journal of Climate Change Strategies and Management Vol 11 No 1, 2019 pp. The full terms of this licence may be seen at http://creativecommons.org/licences/by/4.0/legalcode

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