Fig. 11From: The sensitivity of ocean tide loading displacements to the structure of the upper mantle and crust of Taiwan IslandRMS differences of the modeled M2 OTL displacements between different model combinations. The RMS differences of the modeled M2 OTL displacements are computed between different ocean tide models and FESJB (the Earth model is TW1), as well as between different Earth models and TW1 (the ocean tide model is FESJB)Back to article page