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Variations in Permafrost Temperature and Stability of Alpine Meadows in the Source Area of the Datong River, Northeastern Qinghai‐Tibet Plateau, China
Author(s) -
Li Jing,
Sheng Yu,
Chen Ji,
Wu Jichun,
Wang Shengting
Publication year - 2014
Publication title -
permafrost and periglacial processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.867
H-Index - 76
eISSN - 1099-1530
pISSN - 1045-6740
DOI - 10.1002/ppp.1822
Subject(s) - swamp , permafrost , plateau (mathematics) , vegetation (pathology) , hydrology (agriculture) , environmental science , physical geography , forestry , geography , geology , ecology , biology , medicine , mathematical analysis , mathematics , geotechnical engineering , pathology
Zonal alpine meadow is widespread in the source area of the Datong River, northeastern Qinghai‐Tibet Plateau, China, and can be divided into typical meadow and swamp meadow, according to variations in the soil moisture content. A total of 56 measurements of the mean annual ground temperature (MAGT) revealed a significant difference in the MAGT of the two vegetation types. The measured MAGT varied from ‐2.8 to 0.46°C in the swamp meadow, and from ‐0.6 to 2.5°C in the typical meadow. Measurements of 0°C were found at approximately 3710 m asl and 3660 m asl in the typical meadow and swamp meadow, respectively. Using the measured MAGT and calculated topo‐climatic parameters as dependent and independent variables, two statistical models of MAGT were constructed for each vegetation type. The calculated results were classified into different zones and types to determine the permafrost stability in different vegetated areas. Semi‐stable permafrost (‐3.0°C 0.5°C) were the two main types in the typical meadow. The differences in permafrost temperatures and stability between the two vegetation types can be explained by the local environmental characteristics, including vegetation cover and soil water content. Copyright © 2014 John Wiley & Sons, Ltd.