Surface deformation, gravity and the geoid from a three-dimensional convection model at low Rayleigh numbers
- 23 October 2002
- journal article
- Published by Elsevier
- Vol. 83 (1-4) , 123-136
- https://doi.org/10.1016/0012-821x(87)90056-2
Abstract
No abstract availableKeywords
This publication has 11 references indexed in Scilit:
- Geoid anomalies in a dynamic EarthJournal of Geophysical Research, 1984
- The relationship between surface topography, gravity anomalies, and temperature structure of convectionJournal of Geophysical Research, 1983
- Steady three-dimensional convection at high Prandtl numbersJournal of Fluid Mechanics, 1983
- Mantle convection as a boundary layer phenomenonGeophysical Journal International, 1982
- Kinematic models of large‐scale flow in the Earth's mantleJournal of Geophysical Research, 1979
- Asthenospheric counterflow: a kinematic modelGeophysical Journal International, 1979
- On isostatic geoid anomaliesJournal of Geophysical Research, 1978
- Thermal origin of mid-plate hot-spot swellsGeophysical Journal International, 1978
- Convection in the earth's mantle: towards a numerical simulationJournal of Fluid Mechanics, 1974
- Flow in the Mantle Inferred from the Low Degree Harmonics of the GeopotentialGeophysical Journal of the Royal Astronomical Society, 1967