Global Models From Sparse Data: A Robust Estimate of Earth's Residual Topography Spectrum
A significant component of Earth's surface topography is maintained by stresses induced by underlying mantle flow. This “dynamic” topography cannot be directly observed, but it can be approximated—particularly at longer wavelengths—from measurements of residual topography, which are obtained by...
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Veröffentlicht in: | Geochemistry, geophysics, geosystems : G3 geophysics, geosystems : G3, 2020-08, Vol.21 (8), p.n/a, Article 2020 |
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