“…It is generated mainly by the varying environmental loading throughout the year, but can also be contributed by draconitic period, thermal expansion of ground and monuments, systematic errors or by spurious effects (e.g., Dong et al., 2002; Penna et al., 2007; Ray et al., 2008). On the short‐term temporal‐scale, periodic variations occur as the overtones of seasonal changes, but they are coupled with a plethora of effects due to tidal constituents unmodelled or mismodeled during the processing, GNSS‐specific signals, such as imperfect modeling of orbits, unexpected movement of the GNSS monument, errors in clocks, mismodeling of the large‐scale effects, changes in GNSS processing and errors in the assumptions or background models whose predictions are used during the processing; all these effects will show up in the time series of station displacement (Amiri‐Simkooei et al., 2017; Bos et al., 2015; Dong et al., 2006; Gruszczynski et al., 2018; Langbein & Svarc, 2019; Matviichuk et al., 2020; Niu et al., 2022; Ray et al., 2008; Saji et al., 2020; White et al., 2022; X. Xu et al., 2017; P. Xu et al., 2019). Superposition of the above effects means that the standard deviation of the series may change over the years, and the individual displacements may be correlated with each other.…”