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Climatic regionalisation of continental Chile

机译:智利大陆的气候区域化

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The updated K?ppen–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.
机译:智利大陆更新的K?ppen–Geiger气候分类是对南美环境下的气候研究非常感兴趣的制图产品。这项研究包括200个气象站和气候表面,比例为1:1,500,000。结果表明,智利大陆的气候基本上是干旱(B),温带(C)和极地(E),后者是由于安第斯山脉的海拔升高。主要气候为高苔原(ET)和地中海(Cs)。我们得出的结论是,气候面的使用使新的分类和指数能够随着规模的变化而发展。关于纬度,智利北部的气候因阿塔卡马沙漠而干旱,智利南部的气候为温带气候,从地中海到西海岸。

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