Journal
GEOPHYSICAL JOURNAL INTERNATIONAL
Volume 144, Issue 2, Pages 471-480Publisher
OXFORD UNIV PRESS
DOI: 10.1046/j.1365-246x.2001.00356.x
Keywords
Earth tides; Love number; ocean tides; Q; tides
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The phase lag by which the Earth's body tide follows the tidal potential is estimated for the principal lunar semi-diurnal tide M-2. The estimate results from combining recent tidal solutions from satellite tracking data and from Topex/Poseidon satellite altimeter data. Each data type is sensitive to the body tide lag: gravitationally for the tracking solutions, geometrically for the altimetry. Allowance is made for the lunar atmospheric tide. For the tidal potential Love number k(2), we obtain a lag epsilon of 0.20 degrees +/- 0.05 degrees, implying an effective body tide Q of 280 and body tide energy dissipation of 110+/-25 GW.
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