A new method to determine the upper boundary condition for a permafrost thermal model : an example from the Qinghai-Tibet Plateau
Analyse de régression ; Changement climatique ; Chine ; Climat régional ; Haute montagne ; Infrastructure ; Modèle ; Pergélisol ; Plateau ; Périglaciaire ; Qinghai ; Régime thermique ; Température de l'air ; Température du sol ; Tibet ; Utilisation
Air temperature ; China ; Climatic change ; Cold area ; High mountain ; Infrastructure ; Land use ; Model ; Periglacial features ; Permafrost ; Plateau ; Qinghai ; Regional climate ; Regression analysis ; Soil temperature ; Thermal regime ; Tibet
the scale difference between atmospheric climate models and permafrost thermal models, and allows for a wider range of factors to be used in predicting the thermal boundary condition. For a research site located in Beiluhe, close to the Qinghai-Tibet Railway