Estimation of the 13.63-day lunar tide effect on length of day

Details Estimation of the 13.63-day lunar tide effect on length of day Estimation of the 13.63-day lunar tide effect on length of day

May 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002jgrb..107.2102b&link_type=abstract

Journal of Geophysical Research (Solid Earth), Volume 107, Issue B5, pp. ETG 4-1, CiteID 2102, DOI 10.1029/2000JB000076

Physics

1

Geodesy And Gravity: Rotational Variations, Geodesy And Gravity: Tides-Earth, General Or Miscellaneous: Techniques Applicable In Three Or More Fields

Scientific paper

Using a simple nonlinear analysis method (E. M. Blanter et al., submitted manuscript, 2001), we are able to observe in the length of day the 18.6-year beating of the two main fortnightly lunar tides and to measure the amplitude of the smallest one with a great accuracy. We can thus estimate the associated zonal response coefficient κ for this period. We find κ = 0.311 +/- 0.010.

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