4.2 Article

Climatic regionalisation of continental Chile

Journal

JOURNAL OF MAPS
Volume 13, Issue 2, Pages 66-73

Publisher

TAYLOR & FRANCIS LTD
DOI: 10.1080/17445647.2016.1259592

Keywords

Chile; Koppen-Geiger climatic classification; mediterranean climate; Andes; Atacama Desert; climate surfaces

Funding

  1. Fondecyt Initiation [11130629]
  2. Fondecyt [1150701, 1151087]
  3. Climatology Group at the University of Barcelona (Government of Catalonia) [2014SGR300]
  4. Convenio de Desempeno UTA-MINEDUC

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The 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.

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