Fig. 4From: Determining seasonal displacements of Earth’s crust in South America using observations from space-borne geodetic sensors and surface-loading modelsAnnual amplitudes and phases of a GPS height residuals, b GRACE inverted VCDs, c CLM-GLDAS modeled VCDs, and d CLM-MERRA modeled VCDs. The lengths of the arrows represent the annual amplitudes of the deformations in mm, and the directions present the phases where the peak values of the loadings are counted counterclockwise from the north (January)Back to article page