Fig. 8From: Seasonal and long-term vertical land motion in Southwest China determined using GPS, GRACE, and surface loading modelReason for the difference among the three products. a Relation between the amplitude of gravity recovery and climate experiment (GRACE)-dependent loading deformation and filter radius; b simulative signals of hydrological loading (HYDL) and non-tidal atmospheric loading (NTAL) + non-tidal ocean loading (NTOL); c simulative signals of combined loadingBack to article page