dc.creatorSarricolea Espinoza, Pablo
dc.creatorHerrera Ossandón, Mariajosé
dc.creatorMeseguer Ruiz, Óliver
dc.date.accessioned2018-03-16T17:49:54Z
dc.date.available2018-03-16T17:49:54Z
dc.date.created2018-03-16T17:49:54Z
dc.date.issued2017
dc.identifierJournal of Maps, 2017 Vol. 13, No. 2, 66–73
dc.identifier10.1080/17445647.2016.1259592
dc.identifierhttps://repositorio.uchile.cl/handle/2250/146887
dc.description.abstractThe updated Koppen-Geiger climate classification for continental Chile is a cartographic product of great interest for climate research in the South American context. This study included 200 weather stations and climate surfaces at a scale of 1:1,500,000. The results indicate that the climates of continental Chile are essentially arid (B), temperate (C) and polar (E), the latter due to the elevation of the Andes. The predominant climates are high tundra (ET) and mediterranean (Cs). We have concluded that the use of climate surfaces enables the development of new classifications and indices as a function of scale. With respect to latitude, the climates of northern Chile are arid due to the Atacama Desert, and those of southern Chile are temperate, ranging from mediterranean to marine west coast.
dc.languageen
dc.publisherTaylor & Francis
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Chile
dc.sourceJournal of Maps
dc.subjectChile
dc.subjectKoppen-Geiger climatic classification
dc.subjectMediterranean climate
dc.subjectAndes
dc.subjectAtacama Desert
dc.subjectClimate surfaces
dc.titleClimatic regionalisation of continental Chile
dc.typeArtículo de revista


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