“…Gravity measurement is an effective means to investigate the Earth's interior structures (Blakely, 1996), whose applications range from mining and hydrological problems (Hinderer et al., 2020; Martinez et al., 2012) to geoid determination (Hofmann‐Wellenhof & Moritz, 2006; Philipp et al., 2020) and plate tectonics (Ebbing et al., 2018; Götze & Pail, 2018; Panet et al., 2014). With the emergence of new gravity satellites in the new millennium (Andersen et al., 2010; Floberghagen et al., 2011; Tapley et al., 2004), static and temporal satellite gravity data with unprecedented data coverage and accuracy became easily accessible to geoscientists (Bucha & Janák, 2013; Ince et al., 2019).…”