Error spectrum for the global M₂ ocean tide

Citeable URL: https://ir.library.oregonstate.edu/concern/articles/4x51hp282

Descriptions

Attribute Name	Values
Creator	Ray, Richard D. Eanes, R. J. Egbert, Gary D. Pavlis, N. K.
Abstract	The most accurate determinations of the global ocean tides are currently based on altimeter measurements made by the Topex/Poseidon satellite. The error spectrum corresponding to the M₂ tidal solution is here estimated, primarily by inverse methods and secondarily by simple differencing in flatter than tidal signal spectrum, and it exceeds 10% of the signal at spherical harmonic degree 15 and above. The tide error also exceed the anticipated sensitivity of the upcoming GRACE gravity mission for all degrees below 40, and possibly below 50. Copyrighted by American Geophysical Union.
Resource Type	Article
DOI	https://doi.org/10.1029/2000GL011674
Date Available	2010-04-27T22:34:38+00:00
Date Issued	2001-01-01
Citation	Eanes, R. J., Egbert, G. D., Pavlis, N. K., Ray, R. D., Error spectrum for the global M₂ ocean tide, Geophys. Res. Lett., 28(1), 2001.
Journal Title	Geophysical Research Letters
Journal Volume	28
Journal Issue/Number	1
Rights Statement	Copyright Not Evaluated
Publisher	American Geophysical Union
Language	English [eng]
Replaces	http://hdl.handle.net/1957/15702