hdl:10013/epic.22247
How to Compute Geoid Undulations (Geoid Height Relative to a Given Reference Ellipsoid) from Spherical Harmonic Coefficients for Satellite Altimetry Applications
Contact
mlosch [ at ] awi-bremerhaven.de
Abstract
This document describes in a cookbook-fashion how to obtain geoid height at a given location on the Earth from spherical harmonic coefficients of a gravity model. The document is intended to aid ``the uninitiated oceanographer'' in constructing geoid undulations relative to a given reference ellipsoid, defined by semi-major axis and flattening parameter, to be used with satellite altimetry products.
Item Type
Miscellaneous
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Divisions
AWI Organizations > Climate Sciences > Climate Dynamics
AWI Organizations > Climate Sciences > Physical Oceanography of the Polar Seas
AWI Organizations > Climate Sciences > Sea Ice Physics
AWI Organizations > Climate Sciences > Physical Oceanography of the Polar Seas
AWI Organizations > Climate Sciences > Sea Ice Physics
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Publication Status
Published
Eprint ID
11802
Cite as
Losch, M.
and
Seufer, V.
(2003):
How to Compute Geoid Undulations (Geoid Height Relative to a Given Reference Ellipsoid) from Spherical Harmonic Coefficients for Satellite Altimetry Applications
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