Math 2.0

Geophysics Definition

Physical geodesy

Builds on GeodesyGeopotentialPotential theory

Definition

Physical geodesy is the branch of geodesy that determines the gravity field of the Earth and its relation to the figure of the Earth. Its central unknown is the gravity potential, the geopotential WW, as a function on and outside the Earth's surface. Its methods are those of potential theory, applied to measurements of gravity, of the direction of the plumb line and of satellite orbits.

Remarks

Example: determining the geoid from gravity measurements by Stokes' formula is a problem of physical geodesy. Non-example: computing the distance between two points of a given ellipsoid uses no gravity data; it belongs to geometric geodesy. Physical geodesy also provides orthometric heights, which are measured from the geoid along the plumb line.

Reading path

To understand this page from the ground up, read these 4 pages in order. The foundations come first.

Show the path as a graph
Each page uses the pages above it. The colour of the bar on a box shows how strong the evidence is, and the box also gives it as text. The list has the same pages.
  • no evidence level
  1. Geodesy concept
  2. Geopotential concept
  3. Potential theory concept
  4. Physical geodesy definition

Further reading

  1. Web https://en.wikipedia.org/wiki/Physical_geodesy
About this page
Tag5HE6079K1N
URIm2://5HE6079K1N
Kinddefinition
WritingW0 stub
MSC86A30, 86A20
DefinesPhysical geodesy
UsesGeodesy, Geopotential, Potential theory
Changed3 November 2026

Markdown · JSON · Edit on GitHub

What this page needs for W1

  • an inventory row: the row of the inventory that the node accounts for (0 of 1)
  • a source with a locator (0 of 1)

The writing levels say how complete the text of a page is. They do not measure its truth.

What links here

No page links to this page yet.