AbstractThe ground surface represents the land‐atmosphere interface and plays a crucial role in exchanging energy, matter, and biochemical fluxes. The ground surface temperature (T_s) is hence widely investigated as an indicator to understand the thermal state of soil in a warming world. However, regular and continuous T_s measurements are rare worldwide, and the early T_s records were derived from snow surface measurements and are not comparable with the measurements of modern automatic systems. In this study, we reconstruct the T_s records of the China Meteorological Administration (CMA) for 1956–2022 by numerical simulation. The results show that the mean annual ground surface temperature (MAGST) during 1981–2010 ranged from 0.4 to 30.8°C at 632 stations. The MAGST was mainly controlled by air temperature and refined by snow depth. The overall MAGST increased by 0.20 ± 0.02°C dec⁻¹ across China during 1956–2022 and showed pronounced interdecadal variability corresponding to the surface air temperature (0.23 ± 0.03°C dec⁻¹). At the snow‐covered sites, the T_s warming was amplified by increased snow depth, leading to about 0.24°C dec⁻¹ (or 70.6%) faster warming for T_s in winter compared to that of surface air temperature. Many of the early reported ground surface temperature studies based on CMA measurements did not consider the measurement inconsistency and likely overestimated the warming trend of ground surface temperature over China.