As an intrinsic feature of daily surface air temperature (SAT) variability found in station measurements, temporal asymmetry (TA) can be taken as an evaluation metric to access the quality of SAT re-analysis product. In this study, TA calculated from four SAT variables, i.e., daily mean SAT (T-mean), daily maximum SAT (T-max), daily minimum SAT (T-min) and diurnal temperature range (T-DTR = T-max - T-min), is applied to evaluate synoptic-scale performance of four reanalysis products (NCEP-2, JRA-55, ERA-I, and ERA-5) over China. The results show that four re-analyses overall overestimate the TA of daily T-max and T-min variability over China, but with a comparatively consistent estimated TA for T-mean. Moreover, the TA of T-mean variability for these four re-analyses shares high spatial consistency with those from the observation. However, four re-analyses own the similar region-dependent spatial patterns of overestimated TA for T-max and T-min variability, especially for T-max. Since high TA is an indicator for strong nonlinear feature, only T-mean reanalysis is the most suitable to explore synoptic-scale extreme events, such as heat waves and cold waves, which are highly related to the strong nonlinear processes.