4.6 Article

Thermal Characteristics and Recent Changes of Permafrost in the Upper Reaches of the Heihe River Basin, Western China

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
Volume 123, Issue 15, Pages 7935-7949

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2018JD028442

Keywords

permafrost; seasonally frozen ground; Heihe River Basin; Qilian Mountains

Funding

  1. National Natural Science Foundation of China [91325202]
  2. National Key Scientific Research Program of China [2013CBA01802]
  3. Fundamental Research Funds for the Central Universities [lzujbky_2016_281, 862863]

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To investigate the thermal characteristics and dynamics of permafrost as well as seasonally frozen ground over the upper reaches of the Heihe River Basin (URHR), an observation network with 14 boreholes was established during 2011-2014. The in situ measurements indicated mean annual air temperature that ranged from -5.2 to -2.3 degrees C at the monitored elevation range of approximate to 3,600-4,150m, and mean annual ground surface temperature that ranged from -1.3 to 1.7 degrees C during 2013-2017. The mean annual ground temperature at 16- to 18-m depth ranged from -1.71 degrees C on the high (>4,000 m above sea level) north facing slope to about 0-C around areas near the lower limit of permafrost. Active layer thickness at the monitored sites varied significantly with the range of 0.77-4.90m during 2011-2017, and maximum frozen depth in seasonally frozen ground was about 5m. Permafrost thickness was between approximate to 136m and less than 10m. Both permafrost and seasonally frozen ground were found to be subject to serious warming during the measured period in the URHR. This study provides new quantitative insights for permafrost and seasonally frozen ground in the URHR. Key Points

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