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- W2355171679 abstract "Some problems relevant to the permafrost temperature regime research were analyzed and discussed in this paper, including the lithology of permafrost, water content, configuration and structure, the relationship between surface temperature and air temperature, the heat flow under ground, the determination of research area and some parameters about the lithology, water content, configuration and structure. Based on the research result of some subjects such as analytical physics, geosciences and climatology, some conclusions were drawn as follows: Firstly, in the case of permafrost temperature regime research, the determination of study area should be based on the time scale of research. Because the influence of temperature and heat flow on permafrost in different depths changes with time, the heat flow of permafrost base should be used as the lower boundary condition to solve the problem of permafrost temperature regime. Secondly, Coefficient N, which reflects the relationship between surface temperature and air temperature, changes annually, seasonally and daily. The duration of ground freezing is essential to get the value of the coefficient. Therefore, it is simple to use the value of air temperature minus surface temperature to describe the relationship between them. Thirdly, on account of the diversity of terrain, surface condition, lithology of stratum and heat flow on the Tibetan Plateau, isotherm cannot be used to map permafrost as a single index, and it is unreasonable to forecast permafrost change in accordance with it." @default.
- W2355171679 created "2016-06-24" @default.
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- W2355171679 date "2004-01-01" @default.
- W2355171679 modified "2023-09-24" @default.
- W2355171679 title "Permafrost Temperature Regime: Study Method and Applied Analysis" @default.
- W2355171679 hasPublicationYear "2004" @default.
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