This paper discusses the detection of postglacial rebound by using data from space geodetic measurement of VLBI, and using measuring site velocities and length rates of baselines to detect the vertical and horizontal postglacial rebound respectively. The comparison and correlation analysis between space geodetic results and predictions of postglacial rebound from the geophysical model ICE‐4G shows that they have good agreement, their high correlation coefficients reach to 0.8~0.9, which indicates that the space techniques are now able to detect postglacial rebound at 1~10mm/a level. But in magnitude, space geodetic results are generally 1.2 times larger in absolute value than ICE‐4G predictions, which shows that the current postglacial rebound motion are more violent than the geophysical predictions.