Freeze–thaw cycles and snow impact at arid permafrost region in Chajnantor Volcano, Atacama, northern Chile

Permafrost occurs in the high Atacama Desert, and its thermal state was characterized at a study site 5,075 m a.s.l., at the lower regional altitude boundary for permafrost. The permafrost body is about 5 m thick and located in the hydrothermal alteration zone. The freeze–thaw layer and upper part o...

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Bibliographic Details
Published in:Arctic, Antarctic, and Alpine Research
Main Authors: Gabriela Mena, Kenji Yoshikawa, Norbert Schorghofer, César Pastén, Felipe Agustin Ochoa, Yuzuru Yoshii, Mamoru Doi, Takeshi Miyata, Hidenori Takahashi, Gino Casassa, Toshio Sone
Format: Article in Journal/Newspaper
Language:English
Published: Taylor & Francis Group 2021
Subjects:
permafrost
freeze–thaw cycle
high elevation
atacama
snow
Environmental sciences
GE1-350
Ecology
QH540-549.5
Antarctic and Alpine Research
Arctic
Online Access:https://doi.org/10.1080/15230430.2021.1878739
https://doaj.org/article/7821f2d259eb4f5195f5b60a12e600f9
Description
Summary:Permafrost occurs in the high Atacama Desert, and its thermal state was characterized at a study site 5,075 m a.s.l., at the lower regional altitude boundary for permafrost. The permafrost body is about 5 m thick and located in the hydrothermal alteration zone. The freeze–thaw layer and upper part of the permafrost layer temperatures were measured at 0 to 39 cm depth at 1-cm resolution throughout the year. The upper 3 cm of the ground experienced more than 100 freeze–thaw cycles in 2019. The maximum thaw depth was 14 cm. No significant thermal offset is observed between the annual mean of the surface temperature and the top permafrost boundary. The 14-m borehole reveals that the geothermal gradient was quite high at 200°C/km. In 2019 the seventy days of snow cover impacted the surface energy budget. Winter and summer snow conditions contribute to cooling the surface temperature regime in different ways.

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