In the present study, the alpine meadow ecosystem in the middle and low-latitude permafrost region of the Qinghai–Tibet Plateau (QTP) was selected to examine the impacts of surface soil organic matter on the thermal properties of deep soil.
In the present study, the alpine meadow ecosystem in the middle andlow-latitude permafrost region of the Qinghai–Tibet Plateau (QTP) was selected to examine the impacts ofsurface soil organic matter on the thermal properties of deep soil.