Fig. 6From: The sensitivity of ocean tide loading displacements to the structure of the upper mantle and crust of Taiwan IslandModeled OTL displacements for the M2 tidal harmonic around Taiwan Island. The modeled M2 OTL displacements for the east component (left), north component (middle), and vertical component (right) are computed based on the FESJB ocean tide model and the TW1 Earth modelBack to article page