Minimum, maximum and average amplitudes (mm) of the residuals of the GPS vertical displacement minus predicted OTL, for harmonic M2, at the 26 GPS sites used in this study. The Green's functions are based on earth models S362ANI and STW105, all of them with and without the correction for the anelastic dispersion effects. The ocean tide model used is FES2014b replaced with CIAM2.
Model . | Min . | Max . | Average . |
---|---|---|---|
With anelastic dispersion | |||
S362ANI | 0.14 | 1.79 | 0.75 |
STW105 | 0.06 | 1.92 | 0.84 |
Without anelastic dispersion | |||
S362ANI | 0.42 | 2.27 | 1.18 |
STW105 | 0.53 | 2.41 | 1.31 |
Model . | Min . | Max . | Average . |
---|---|---|---|
With anelastic dispersion | |||
S362ANI | 0.14 | 1.79 | 0.75 |
STW105 | 0.06 | 1.92 | 0.84 |
Without anelastic dispersion | |||
S362ANI | 0.42 | 2.27 | 1.18 |
STW105 | 0.53 | 2.41 | 1.31 |
Minimum, maximum and average amplitudes (mm) of the residuals of the GPS vertical displacement minus predicted OTL, for harmonic M2, at the 26 GPS sites used in this study. The Green's functions are based on earth models S362ANI and STW105, all of them with and without the correction for the anelastic dispersion effects. The ocean tide model used is FES2014b replaced with CIAM2.
Model . | Min . | Max . | Average . |
---|---|---|---|
With anelastic dispersion | |||
S362ANI | 0.14 | 1.79 | 0.75 |
STW105 | 0.06 | 1.92 | 0.84 |
Without anelastic dispersion | |||
S362ANI | 0.42 | 2.27 | 1.18 |
STW105 | 0.53 | 2.41 | 1.31 |
Model . | Min . | Max . | Average . |
---|---|---|---|
With anelastic dispersion | |||
S362ANI | 0.14 | 1.79 | 0.75 |
STW105 | 0.06 | 1.92 | 0.84 |
Without anelastic dispersion | |||
S362ANI | 0.42 | 2.27 | 1.18 |
STW105 | 0.53 | 2.41 | 1.31 |
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