Pedoclimate monitoring in the periglacial high mountain soils of the Atacama Desert, northern Chile

Pedoclimate monitoring in the Central Andes is key to understanding climatic change in arid high‐mountain low‐latitude environments. We carried out a study of the thermal–hydric regimes of three soils along an altitudinal gradient in the Licancabur Volcano, northern Chile. In situ measurements of so...

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