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Fig. 8 | Earth, Planets and Space

Fig. 8

From: Seasonal and long-term vertical land motion in Southwest China determined using GPS, GRACE, and surface loading model

Fig. 8

Reason 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 loading

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