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dc.contributor.authorPisabarro Pérez, Alfonso
dc.contributor.authorPellitero Ondicol, Ramón
dc.contributor.authorSerrano Cañadas, Enrique 
dc.contributor.authorGómez Lende, Manuel
dc.contributor.authorGonzález Trueba, Juan José
dc.date.accessioned2020-03-23T13:33:14Z
dc.date.available2020-03-23T13:33:14Z
dc.date.issued2017
dc.identifier.citationCatena, 2017, vol. 149, part 2. p. 623-636es
dc.identifier.issn0341-8162es
dc.identifier.urihttp://uvadoc.uva.es/handle/10324/40681
dc.descriptionProducción Científicaes
dc.description.abstractGround temperatures determine significant geomorphological processes in a wet and temperate mountain with a narrow high elevation range belt. Twenty five temperature data loggers were buried at a shallow depth in different locations and altitudes and at specifically cold locations at two massifs in the Cantabrian Mountains (North Spain), Picos de Europa and Fuentes Carrionas. This paper analyses the ground thermal regime and associated parameters (e.g. freeze index, duration and depth of freeze, freeze and thaw cycles) and correlates them with active geomorphological processes and landforms. The thermal regime varies in accordance to the topoclimatic conditions, and it was possible to determinate annual phases in function of snow cover behaviour. Main active processes and landforms stop their activity with a large snow cover which thermally protects the ground and in consequence, avoids the freeze and thaw cycles. During this period, the records allow to asseverate the evidence of seasonal freeze grounds in several locations. Permafrost was not discover on the ground at any of the thermometers except one located at the vicinity of a relict ice patch. With the help of geomorphological maps and previous works, we got to establish the relation between geomorphological processes, landforms, snow cover and ground thermal regime.es
dc.format.mimetypeapplication/pdfes
dc.language.isoenges
dc.publisherElsevieres
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectGeomorfología - España - Cordillera Cantábricaes
dc.subject.classificationGround thermal regimees
dc.subject.classificationRégimen térmico de sueloses
dc.subject.classificationLandformses
dc.subject.classificationAccidentes geográficoses
dc.subject.classificationGeomorphological processeses
dc.subject.classificationProcesos geomorfológicoses
dc.titleGround temperatures, landforms and processes in an Atlantic mountain. Cantabrian Mountains (Northern Spain)es
dc.typeinfo:eu-repo/semantics/articlees
dc.rights.holder© 2017 Elsevieres
dc.identifier.doi10.1016/j.catena.2016.07.051es
dc.relation.publisherversionhttps://www.sciencedirect.com/science/article/abs/pii/S0341816216303101es
dc.peerreviewedSIes
dc.description.projectMinisterio de Educación y Formación Profesional (project FPU13/05837)es
dc.description.projectOrganismo Autónomo Parques Nacionales - Ministerio de Agricultura y Pesca, Alimentación y Medio Ambiente (project OAPN 053/2010)es
dc.description.projectMinisterio de Economía, Industria y Competitividad (project CGL2015-68144-R)es
dc.description.projectLeverhulme Trust International Network (grant IN-2012-140)es
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.type.hasVersioninfo:eu-repo/semantics/submittedVersiones


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