The trend of wetting or drying is an important metric of regional and global climate change. Based on daily meteorological data during 1951–2018 from 10 stations in arid regions of North China, the performances of two indicators, relative humidity (RH) and actual water vapour pressure (e_a), in evaluating the trends of air humidification are investigated. Results show that annual RH decreases by 0–0.10% yr⁻¹ during the past decades in almost all (90%) stations, whereas annual e_a presents increasing trends in 40% of stations and decreasing trends in the other 60% stations. Therefore, contrasting results are observed in the trends of air humidity reflected RH and e_a. Specifically, stations getting significantly drying as indicated by RH, it is tend to getting less drying or even wetting as indicated by e_a. These results suggest that it tend to give a misleading conclusion with the trends of RH as indicator in evaluating the trends of regional or global wetting or drying, due to the reduction in RH caused by the accompanying temperature rising under global warming. The other indicator e_a is more consistent with the precipitation changes, and suitable for trending analyses of air humidification under such circumstance. Further researches should be done in a larger scale arid region and in different seasons, to investigate the differences in the trends of air humidification indicated by RH and e_a, and discuss the response of the changes of wetting or drying to the varied meteorological factors.