利用ＧＡＭＥ－ Ｔｉｂｅｔ 野外观测期间所得藏北高原不同地点土壤温度资料， 对藏北高原土壤温度分布纬向地带性和垂直地带性特征进行分析， 结果表明夏季土壤温度分布主要表现为高度效应，而冬季土壤温度分布主要表现为纬度效应。年平均土壤温度分布是纬度效应和高度效应综合作用的结果。 Based on the data of soil temperature at different sites in the GAME-Tibet field during the field observation, the zonal and vertical zonal characteristics of soil temperature distribution in the northern Tibet Plateau were analyzed. The results showed that the soil temperature distribution in summer mainly showed a height effect, while in winter Soil temperature distribution is mainly manifested as latitude effect. The annual average soil temperature distribution is the result of a combination of latitude and altitude effects.