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Inexistence of permafrost at the top of the Veleta peak (Sierra Nevada, Spain)

dc.contributor.authorOliva, Marc
dc.contributor.authorGómez-Ortiz, A.
dc.contributor.authorSalvador-Franch, F.
dc.contributor.authorSalvà-Catarineu, M.
dc.contributor.authorPalacios, D.
dc.contributor.authorTanarro, L.
dc.contributor.authorRamos, M.
dc.contributor.authorPereira, P.
dc.contributor.authorRuiz-Fernández, J.
dc.date.accessioned2017-06-26T10:10:52Z
dc.date.available2017-06-26T10:10:52Z
dc.date.issued2016
dc.description.abstractA 114.5m deep drilling was carried out in August 2000 in the bedrock of the Veleta peak, at 3380m in the massif of Sierra Nevada, Southern Spain. The objective of this work is to analyse temperatures at the first 60m depth of this drilling from September 2002 to August 2013 based on 11 UTL-1 thermal loggers located at different depths, together with air temperatures at the summit of the Veleta peak. Permanent negative temperatures have not been detected in the borehole, which shows evidence of the absence of widespread permafrost conditions nowadays in the highest lands of this massif. Bedrock temperatures oscillated between 3.2°C at 0.6m depth and 2°C at 20m below the surface. The largest temperature ranges were recorded on the most external sensors until 1.2m depth, where values reached 22.3°C. Seasonal temperature variations were significant until 10m depth. The thickness of the seasonal frozen layer was highly variable (0.6-2m) and dependent on annual climate conditions. The mean air temperature at the Veleta peak increased by 0.12°C during the study period. Bedrock temperatures followed diverging trends: a drop of 0.3-0.4°C down to 0.6m depth, a decrease of up to 0.7°C between 4 and 10m, thermal stability at 20m and a rise of 0.2°C that occurred in 2009 at the deepest sensor at 60m. The calculation of the thermal wave damping in the subsoil of the Veleta peak has allowed for quantifying the thermal diffusivity of the rock as (7.05±0.03)10(-7)m(2)/s, which means that the external climate signal arrives with an 8.5-year lag to the sensor at 60m deep. This allows to deduce a trend change in the climate of the area, moving from warmer conditions towards a trend of cooling from 2006 to 2007.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationOliva, Marc, Gómez-Ortiz, A., Salvador-Franch, F., Salvà-Catarineu, M., Palacios, D., Tanarro, L., Ramos, M., Pereira, P., & Ruiz-Fernández, J. (2016). Inexistence of permafrost at the top of the Veleta peak (Sierra Nevada, Spain). Science of The Total Environment, 550, 484–494. https://doi.org/10.1016/j.scitotenv.2016.01.150pt_PT
dc.identifier.doi10.1016/j.scitotenv.2016.01.150pt_PT
dc.identifier.issn0048-9697
dc.identifier.urihttp://hdl.handle.net/10451/28172
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherElsevierpt_PT
dc.subjectPACE projectpt_PT
dc.subjectSierra Nevadapt_PT
dc.subjectGround temperaturespt_PT
dc.subjectAir temperaturespt_PT
dc.titleInexistence of permafrost at the top of the Veleta peak (Sierra Nevada, Spain)pt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.endPage494pt_PT
oaire.citation.startPage484pt_PT
oaire.citation.titleScience of the Total Environmentpt_PT
oaire.citation.volume550pt_PT
person.familyNameOliva
person.familyNameRamos
person.givenNameMarc
person.givenNameMiguel
person.identifier.ciencia-id5510-AC71-085A
person.identifier.orcid0000-0001-6521-6388
person.identifier.orcid0000-0003-3648-6818
person.identifier.ridK-5423-2014
person.identifier.ridK-2230-2014
person.identifier.scopus-author-id35225198700
person.identifier.scopus-author-id8676487200
rcaap.rightsclosedAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublicationd416bf65-77f6-488e-b275-5fbb257df6d4
relation.isAuthorOfPublicationa0544f42-b78e-4fd4-9204-f6acfa4e1e9d
relation.isAuthorOfPublication.latestForDiscoveryd416bf65-77f6-488e-b275-5fbb257df6d4

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