Earth Surface Relationships
The geoid is a gravity equipotential surface selected to match mean sea level as well as possible.
For more on this see NIMA’s “Geodesy for the Layman” on
http://164.214.2.59/geospatial/products/GandG/geolay/toc.htm
• h is the geodetic height
• H is the orthometric height
• N is the separation of the geoid