Fig. 3From: Seasonal and long-term vertical land motion in Southwest China determined using GPS, GRACE, and surface loading modelLoading components in Southwest China. Stack-average deformation of 41 stations yielded by hydrological loading (HYDL), non-tidal atmospheric loading (NTAL), and non-tidal ocean loading (NTOL) represented by the blue, red, and green lines, respectively [inferred from the surface loading model (SLM)]Back to article page