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dc.contributor.authorSerra, Teresaes_ES
dc.contributor.authorPascual, Josepes_ES
dc.contributor.authorBrunet, Ramones_ES
dc.contributor.authorColomer, Jordies_ES
dc.date.accessioned2020-08-19T08:32:44Z-
dc.date.available2020-08-19T08:32:44Z-
dc.date.issued2020-06-
dc.identifier.citationWater 12(6): 1621 (2020)es_ES
dc.identifier.otherCEX2019-000928-S-
dc.identifier.urihttp://hdl.handle.net/10261/218214-
dc.descriptionSpecial Issue Climate Change Effects on Hydrological Processes, Water Resources, Ecosystems and Agriculture.-- 12 pages, 5 figureses_ES
dc.description.abstractThis study analyses the water temperature changes in Lake Banyoles over the past four decades. Lake Banyoles, Spain’s second highest lake, situated in the western Mediterranean (NE Iberian Peninsula). Over the past 44 years, the warming trend of the lake’s surface waters (0.52 °C decade−1) and the cooling trend of its deep waters (−0.66 °C decade−1) during summer (July–September) have resulted in an increased degree of stratification. Furthermore, the stratification period is currently double that of the 1970s. Meanwhile, over the past two decades, lake surface turbidity has remained constant in summer. Although turbidity did decrease during winter, it still remained higher than in the summer months. This reduction in turbidity is likely associated with the decrease in groundwater input into the lake, which has been caused by a significant decrease in rainfall in the aquifer recharge area that feeds the lake through groundwater sources. As a unique freshwater sentinel lake under the influence of the climate change, Lake Banyoles provides evidence that global warming in the western Mediterranean boosts the strength and duration of the lake’s stratification and, in response, the associated decrease in the turbidity of its epilimniones_ES
dc.description.sponsorshipThis study was funded by Aigües de Banyoles (AB-UDG/2020/1)es_ES
dc.description.sponsorshipWith the funding support of the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S), of the Spanish Research Agency (AEI)-
dc.language.isoenges_ES
dc.publisherMultidisciplinary Digital Publishing Institutees_ES
dc.relation.isversionofPublisher's versiones_ES
dc.rightsopenAccesses_ES
dc.subjectClimate changees_ES
dc.subjectTurbidityes_ES
dc.subjectLake mixing regimees_ES
dc.subjectHydrothermal turbid plumeses_ES
dc.subjectRainfalles_ES
dc.titleThe Mixing Regime and Turbidity of Lake Banyoles (NE Spain): Response to Climate Changees_ES
dc.typeartículoes_ES
dc.identifier.doi10.3390/w12061621-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttps://doi.org/10.3390/w12061621es_ES
dc.identifier.e-issn2073-4441-
dc.rights.licensehttps://creativecommons.org/licenses/by/4.0/es_ES
dc.contributor.funderAigües de Banyoleses_ES
dc.contributor.funderAgencia Estatal de Investigación (España)-
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
dc.identifier.funderhttp://dx.doi.org/10.13039/501100011033es_ES
dc.subject.urihttp://metadata.un.org/sdg/13es_ES
dc.type.coarhttp://purl.org/coar/resource_type/c_6501es_ES
dc.subject.sdgTake urgent action to combat climate change and its impactses_ES
item.openairetypeartículo-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
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