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dc.contributor.authorMoutahir, Hassane
dc.contributor.authorBellot Pujalte, Pau
dc.contributor.authorMonjo, Robert
dc.contributor.authorBellot, Juan
dc.contributor.authorGarcía Ferrandez, Miguel Antonio
dc.contributor.authorTouhami, Issam
dc.date.accessioned2017-04-27T19:44:41Z
dc.date.issued2016-12-29
dc.identifier.citationMoutahir, H., Bellot, P., Monjo, R., Bellot, J., García, M., Touhami, I. Likely effects of climate change on groundwater availability in a Mediterranean region of Southeastern Spain. "Hydrological processes", 29 Desembre 2016, vol. 31, núm. 1, p. 161-176.
dc.identifier.issn0885-6087
dc.identifier.urihttp://hdl.handle.net/2117/103821
dc.description.abstractGroundwater resources are typically the main fresh water source in arid and semi-arid regions. Natural recharge of aquifers is mainly based on precipitation; however, only heavy precipitation events (HPEs) are expected to produce appreciable aquifer recharge in these environments. In this work, we used daily precipitation and monthly water level time series from different locations over a Mediterranean region of Southeastern Spain to identify the critical threshold value to define HPEs that lead to appreciable aquifer recharge in this region. Wavelet and trend analyses were used to study the changes in the temporal distribution of the chosen HPEs (=20¿mm¿day-1) over the observed period 1953–2012 and its projected evolution by using 18 downscaled climate projections over the projected period 2040–2099. The used precipitation time series were grouped in 10 clusters according to similarities between them assessed by using Pearson correlations. Results showed that the critical HPE threshold for the study area is 20¿mm¿day-1. Wavelet analysis showed that observed significant seasonal and annual peaks in global wavelet spectrum in the first sub-period (1953–1982) are no longer significant in the second sub-period (1983–2012) in the major part of the ten clusters. This change is because of the reduction of the mean HPEs number, which showed a negative trend over the observed period in nine clusters and was significant in five of them. However, the mean size of HPEs showed a positive trend in six clusters. A similar tendency of change is expected over the projected period. The expected reduction of the mean HPEs number is two times higher under the high climate scenario (RCP8.5) than under the moderate scenario (RCP4.5). The mean size of these events is expected to increase under the two scenarios. The groundwater availability will be affected by the reduction of HPE number which will increase the length of no aquifer recharge periods (NARP) accentuating the groundwater drought in the region. Copyright © 2016 John Wiley & Sons, Ltd.
dc.format.extent16 p.
dc.language.isoeng
dc.subjectÀrees temàtiques de la UPC::Enginyeria civil::Geologia::Hidrologia subterrània
dc.subject.lcshGroundwater drought
dc.subject.otherheavy precipitation events
dc.subject.otheraquifer recharge
dc.subject.otherwavelet transform
dc.subject.othertrends
dc.subject.othergroundwater drought
dc.subject.otherclimate change
dc.titleLikely effects of climate change on groundwater availability in a Mediterranean region of Southeastern Spain
dc.typeArticle
dc.subject.lemacAigües subterrànies -- Recàrrega
dc.identifier.doi10.1002/hyp.10988
dc.description.peerreviewedPeer Reviewed
dc.relation.publisherversionhttp://onlinelibrary.wiley.com/doi/10.1002/hyp.10988/full
dc.rights.accessRestricted access - publisher's policy
local.identifier.drac19697057
dc.description.versionPostprint (published version)
dc.date.lift10000-01-01
local.citation.authorMoutahir, H.; Bellot, P.; Monjo, R.; Bellot, J.; García, M.; Touhami, I.
local.citation.publicationNameHydrological processes
local.citation.volume31
local.citation.number1
local.citation.startingPage161
local.citation.endingPage176


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