Thermal state of the active layer and permafrost along the Qinghai-Xizang (Tibet) Railway from 2006 to 2010

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Abstract

In this study, we investigated changes in active layer thickness (ALT) and permafrost temperatures at different depths using data from the permafrost monitoring network along the Qinghai-Xizang (Tibet) Railway (QXR) since 2005. Among these sites, mean ALT is ∼3.1 m, with a range of ∼1.1 to 5.9 m. From 2006 through 2010, ALT has increased at a rate of ∼6.3 cm a -1. The mean rate of permafrost temperature rise at the depth of 6.0 m is ∼0.02 °C a-1, estimated by linear regression using 5 yr of data, and the mean rate of mean annual ground temperature (MAGT) rise at a depth of zero amplitude is ∼0.012 °C a-1. Changes for colder permafrost (MAGT -1.0 °C). This is consistent with results observed in the Arctic and subarctic. © 2012 Author(s).

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Wu, Q., Zhang, T., & Liu, Y. (2012). Thermal state of the active layer and permafrost along the Qinghai-Xizang (Tibet) Railway from 2006 to 2010. Cryosphere, 6(3), 607–612. https://doi.org/10.5194/tc-6-607-2012

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