The deflection of the vertical (DOV), the angle at a given point on the Earth between the vertical and the direction of the normal to the reference ellipsoid through that point (Herrmann and Bucksch, 2014), is critical to different directions (Barzaghi et al., 2016) in geodesy, for example, the transformation between astronomical and geodetic results including coordinates and azimuth angles, the transformation between different height systems, the reduction of horizontal and vertical angles to an ellipsoid surface, geodetic net calculations and geoid detection. Some critical applications of the DOV and its variation, that is, plumb line variations (Li and Li, 2009;Li et al., 2001;Tanaka et al., 2001), probably are national defense, aerospace applications, and geophysics research. In particular, geophysics can reveal the migration of materials underground, which has a significant impact on embodied earthquake signal analysis and could contribute to earthquake monitoring. Both the International Astronomical Union and the International Association of Geodesy pay considerable attention to studying the DOV.The methods for determining the DOV include astro-and geodetic observations. For example, the observation equipment has been updated from traditional astronomical theodolite or zenith tubes to digital zenith telescopes in recent years (which have an absolute axis pointing error of 1 E 2ʺ and 0.2ʺ observing internal coincidence, respectively); other methods include early global navigation satellite system (GNSS) and leveling measurements (e.g., 0.7ʺ calculation accuracy could be obtained using the geoid in an accuracy level of several centimeters), which are available for small and linear terrain features (Ceylan, 2009), and gravitational methods (e.g., the mean accuracy of the DOV in the 2000 China gravitational field and quasi-geoid system ([CGGM] could reach up to 1.5ʺ [Sun et al., 2005]).