The Surface Energy Budget and Its Impact on the Freeze-thaw Processes of Active Layer in Permafrost Regions of the Qinghai-Tibetan Plateau

• Published in: Advances in atmospheric sciences 2022, Vol.39 (1), p.189-200
• Main Authors: Ma, Junjie, Li, Ren, Liu, Hongchao, Huang, Zhongwei, Wu, Tonghua, Hu, Guojie, Xiao, Yao, Zhao, Lin, Du, Yizhen, Yang, Shuhua
• Format: Article
• Language: English
• Subjects: Active layer; Albedo; Albedo (solar); Atmospheric Sciences; Cold season; Earth and Environmental Science; Earth Sciences; Energy; Energy budget; Energy distribution; Energy flux; Energy transfer; Enthalpy; Fluctuations; Freeze-thaw; Freeze-thawing; Geophysics/Geodesy; Heat balance; Heat flux; Heat transfer; Latent heat; Latent heat flux; Meteorology; Moisture content; Net radiation; Original Paper; Permafrost; Radiation balance; Seasonal variation; Seasonal variations; Seasons; Sensible heat; Sensible heat flux; Sensible heat transfer; Snow; Snow cover; Soil; Soil heat flux; Soil investigations; Soil layers; Soil moisture; Soil moisture content; Soil surfaces; Surface energy; Surface properties; Temperature; Warm seasons; Water content
• ISSN: 0256-1530; 1861-9533
• DOI: 10.1007/s00376-021-1066-2

The surface energy budget is closely related to freeze-thaw processes and is also a key issue for land surface process research in permafrost regions. In this study, in situ data collected from 2005 to 2015 at the Tanggula site were used to analyze surface energy regimes, the interaction between surface energy budget and freeze-thaw processes. The results confirmed that surface energy flux in the permafrost region of the Qinghai-Tibetan Plateau exhibited obvious seasonal variations. Annual average net radiation ( R n ) for 2010 was 86.5 W m −2 , with the largest being in July and smallest in November. Surface soil heat flux ( G 0 ) was positive during warm seasons but negative in cold seasons with annual average value of 2.7 W m −2 . Variations in R n and G 0 were closely related to freeze-thaw processes. Sensible heat flux ( H ) was the main energy budget component during cold seasons, whereas latent heat flux (LE) dominated surface energy distribution in warm seasons. Freeze-thaw processes, snow cover, precipitation, and surface conditions were important influence factors for surface energy flux. Albedo was strongly dependent on soil moisture content and ground surface state, increasing significantly when land surface was covered with deep snow, and exhibited negative correlation with surface soil moisture content. Energy variation was significantly related to active layer thaw depth. Soil heat balance coefficient K was > 1 during the investigation time period, indicating the permafrost in the Tanggula area tended to degrade.