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Fig. 3 | Earth, Planets and Space

Fig. 3

From: The sensitivity of ocean tide loading displacements to the structure of the upper mantle and crust of Taiwan Island

Fig. 3

Differences between the original and perturbed displacement Green’s functions. The differences of displacement Green’s functions for the horizontal (left) and vertical (right) components to + 1% linear perturbations of the bulk modulus (red), shear modulus (green), and density (blue) in the upper crust at depths of 0–13.88 km (top row), the middle crust at depths of 13.88–24.52 km (second row), the lower crust at depths of 24.52–32.15 km (third row), and the region above the LVZ (LID) at depths of 32.15–80 km (bottom row) separately from TW1 as a function of angular distance. The displacement Green’s functions are scaled by 1012 in the CE frame, where R is the radius of the Earth and θ is the angular distance

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