Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.11765/12179
Elevation effects on air temperature in a topographically complex mountain valley in the Spanish Pyrenees
Full metadata record
DC FieldValueLanguage
dc.contributor.authorNavarro-Serrano, F.es_ES
dc.contributor.authorLópez Moreno, Juan Ignacioes_ES
dc.contributor.authorAzorín Molina, Césares_ES
dc.contributor.authorAlonso-González, E.es_ES
dc.contributor.authorAznárez-Balta, M.es_ES
dc.contributor.authorBuisán, Samueles_ES
dc.contributor.authorRevuelto, Jesúses_ES
dc.date.accessioned2020-06-23T13:33:48Z-
dc.date.available2020-06-23T13:33:48Z-
dc.date.issued2020-
dc.identifier.citationAtmosphere. 2020, 11(6), 656es_ES
dc.identifier.issn2073-4433-
dc.identifier.urihttp://hdl.handle.net/20.500.11765/12179-
dc.description.abstractAir temperature changes as a function of elevation were analyzed in a valley of the Spanish Pyrenees. We analyzed insolation, topography and meteorological conditions in order to understand how complex topoclimatic environments develop. Clustering techniques were used to define vertical patterns of air temperature covering more than 1000 m of vertical elevation change. Ten locations from the bottom of the valley to the summits were monitored from September 2016 to June 2019. The results show that (i) night‐time lapse rates were between −4 and −2 °C km−1, while in the daytime they were from −6 to −4 °C km−1, due to temperature inversions and topography. Daily maximum temperature lapse rates were steeper from March to July, and daily minimum temperatures were weaker from June to August, and in December. (ii) Different insolation exposure within and between the two analyzed slopes strongly influenced diurnal air temperatures, creating deviations from the general lapse rates. (iii) Usually, two cluster patterns were found (i.e., weak and steep), which were associated with stable and unstable weather conditions, respectively, in addition to high‐low atmospheric pressure and low‐high relative humidity. The results will have direct applications in disciplines that depend on air temperature estimations (e.g., snow studies, water resources and sky tourism, among others).es_ES
dc.description.sponsorshipThis study was funded by the Spanish Ministry of Economy and Competitiveness project CGL2017‐82216‐R (HIDROIBERNIEVE).es_ES
dc.language.isoenges_ES
dc.publisherMultidisciplinary Digital Publishing Institutees_ES
dc.rightsLicencia CC: Reconocimiento CC BYes_ES
dc.subjectAir temperaturees_ES
dc.subjectComplex terraines_ES
dc.subjectCluster analysises_ES
dc.subjectLapse rateses_ES
dc.subjectWeather typeses_ES
dc.titleElevation effects on air temperature in a topographically complex mountain valley in the Spanish Pyreneeses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherversionhttps://dx.doi.org/10.3390/atmos11060656es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
Appears in Collections:Artículos científicos 2019-2021


Files in This Item:
  File Description SizeFormat 
atmosphere-11-00656.pdf
3,11 MBAdobe PDFThumbnail
View/Open
Show simple item record



Items in Arcimís are protected by Creative Commons License, unless otherwise indicated.

Arcimís Repository
Nota Legal Contacto y sugerencias