2007
DOI: 10.1002/hyp.6620
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The effects of climate change on potential groundwater recharge in Great Britain

Abstract: The predicted increase in mean global temperature due to climate change is expected to affect water availability and, in turn, cause both environmental and societal impacts. To understand the potential impact of climate change on future sustainable water resources, this paper outlines a methodology to quantify the effects of climate change on potential groundwater recharge (or hydrological excess water) for three locations in the north and south of Great Britain. Using results from a stochastic weather generat… Show more

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Cited by 110 publications
(57 citation statements)
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“…Arnell, 1999a,b;Guo et al, 2002;Tate et al, 2004;Leander & Buishand, 2007;Linderink et al, 2007;Herrera-Pantoja & Hiscock, 2008) yet our results show that this approach can substantially underestimate groundwater recharge. The assumption of a constant relationship between modelled and historical precipitation under future climatic conditions is, however, a source of uncertainty with the transformation approach.…”
Section: Transformed Precipitation-derived Groundwater Recharge and Rmentioning
confidence: 48%
“…Arnell, 1999a,b;Guo et al, 2002;Tate et al, 2004;Leander & Buishand, 2007;Linderink et al, 2007;Herrera-Pantoja & Hiscock, 2008) yet our results show that this approach can substantially underestimate groundwater recharge. The assumption of a constant relationship between modelled and historical precipitation under future climatic conditions is, however, a source of uncertainty with the transformation approach.…”
Section: Transformed Precipitation-derived Groundwater Recharge and Rmentioning
confidence: 48%
“…Predicting the dynamics and processes interactions affecting groundwater recharge over time requires a reliable prediction of critical climate variables Herrera-Pantoja and Hiscock 2008;Jyrkama and Sykes 2007). Recharge occurs via two general pathways in many environments: diffuse recharge to the water table and focused recharge that occurs at locations where surface-water flow is concentrated at the land surface, including stream channels, lakes, topographic depressions, irrigated-agricultural land, and other macropore, preferential-flow pathways (Small 2005).…”
Section: Groundwater Rechargementioning
confidence: 99%
“…Eckhardt and Ulbrich [12] from their study on the Dill catchment in south east Germany, suggest that recharge rates could be as low as 50% of the existing values, whereas Herrera-Pantoja and Hiscock [13] from their study in three locations (Coltishall, Gatwick and Paisley)in UK conclude that recharge rates could be as low as 88% of the existing rates at least for Paisley and in general it will be declining with the increase of temperatures. Thampi and Raneesh [18], from their study in Chaliyar river basin in Kerala, South India forecast a reduction of recharge by 4 -7% by 2071-2100.…”
Section: Introductionmentioning
confidence: 96%
“…In the last century, the temperature of the earth rose by about 0.6C [4] and it is expected to rise between 1.4 to 5.8C by 2100 due to the emission of greenhouse gasses [5] and the temperature in Sri Lanka is said to increase by 0.9 -4.0C by 2100 over the baseline period temperature [6]. Worldwide, there have been many studies related to various aspects of climate change on groundwater [7,8,9,10] and a relatively fair number of studies on the effect of climate change on the groundwater recharge [11,12,13,14,15,16,17,18]. However, the 4 th report of IPCC [19] states that "there has been very little research on the impact of climate change on groundwater and that the few studies of climatic impacts on groundwater for various aquifers show very site specific results".…”
Section: Introductionmentioning
confidence: 99%