Undulation Of The Geoid

Somewhat old-fashioned name for the separation N between the geoid and the reference ellipsoid of the Earth. Because geophysical heights H "above sea level" refer to the geoid, but GPS positioning provides in a direct geometric fashion heights h above the GRS80 reference ellipsoid, it has become a matter of great importance to determine accurate representations, or maps, of geoid undulations N = h -H,\, over the territories of nations, to allow the inexpensive GPS technology to be harnessed for the precise determination of heights.

 

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