Because snow cover is one of the most active elements of the cryosphere, snow monitoring is important for blizzard monitoring, hydrological forecasting, and climate change studies. In September 2015, we established an automatic network of ten stations to continuously measure the snow depth on the Tibetan Plateau. Each station is equipped with an SR50A sonic ranging sensor and a Hydra Probe II soil sensor to measure snow depth, soil moisture, and other soil properties in near real time. The accuracy of the snow depth and soil moisture of this dataset reaches about 1 cm and 3%, respectively. This dataset will be helpful for snow disaster monitoring and the evaluation of snow cover products derived from satellites.