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Temperature trends
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dc.contributor.authorGuijarro Pastor, José Antonioes_ES
dc.date.accessioned2017-08-02T07:50:48Z-
dc.date.available2017-08-02T07:50:48Z-
dc.date.issued2013-
dc.identifier.urihttp://hdl.handle.net/20.500.11765/7375-
dc.description.abstractMean maximum and minimum monthly temperatures have been collected for all stations with at least 10 years of observations during the period 1951-2012. 2856 series were compiled in total, which were homogenized with the R package “Climatol”. Trends of the homogenized series were computed by linear regression with time, whose greater positive values were obtained in summer and spring, but with differing patterns in the main hydrological basins. Maximum temperature trends were negative in the Canary Islands only. Geographical distribution of trends and dependence with altitude have been studied, the higher trends corresponding to the eastern third of the Iberian peninsula and Tajo river basin.es_ES
dc.language.isoenges_ES
dc.publisherDelegación Territorial en Illes Balearses_ES
dc.rightsLicencia CC: Reconocimiento–NoComercial–SinObraDerivada CC BY-NC-NDes_ES
dc.subjectHomogenizationes_ES
dc.subjectTemperature serieses_ES
dc.subjectTrendses_ES
dc.subjectDTRes_ES
dc.titleTemperature trendses_ES
dc.typeinfo:eu-repo/semantics/otheres_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
Colecciones: AEMET - Estudios


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