Geophysics Gravity field of the Earth Problem
Molodensky's problem
Builds on GeopotentialHarmonic function
Problem
Let be the known angular velocity of the Earth about the -axis, and let be the centrifugal potential. Let be the unit sphere, used as a parameter set, and suppose the values and are given for every . Find a closed surface in , given by an embedding , and a function harmonic outside with as . They must be such that the geopotential satisfies Here comes from levelling combined with gravity, and the direction of from astronomical latitude and longitude.
Remarks
Unlike the geodetic boundary value problem in Stokes' form, the boundary surface is an unknown, so this is a free boundary problem for the Laplace equation. It avoids any hypothesis about the masses between the geoid and the surface, which Stokes' approach needs. In practice it is linearised around a known approximate surface, and the linear problem is solved by series or integral equation methods. Lars Hörmander proved in 1976 a local existence and uniqueness theorem for the nonlinear problem, for data close to those of a reference solution, using a Nash–Moser iteration.
Reading path
To understand this page from the ground up, read these 14 pages in order. The foundations come first.
Show the path as a graph
- no evidence level
- Euclidean space object
- Function concept
- Geopotential concept
- Total derivative concept
- Function of several variables concept
- Vector-valued function concept
- Differentiable function of several variables concept
- Partial derivative concept
- Vector field concept
- Gradient concept
- Divergence concept
- Laplacian concept
- Harmonic function concept
- Molodensky's problem problem
Further reading
About this page
| Tag | PHW0E57MH3 |
|---|---|
| URI | m2://PHW0E57MH3 |
| Kind | problem |
| Writing | W0 stub |
| MSC | 86A30, 31B20, 35R35 |
| Status | This copy of the site has no build data. Run m2 status PHW0E57MH3. |
| About | Geopotential |
| Uses | Geopotential, Harmonic function |
| Changed | 3 November 2026 |
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