CONSTRAINTS ON ENERGY DISSIPATION IN THE EARTH'S BODY TIDE FROM SATELLITE TRACKING AND ALTIMETRY

dc.contributor.authorRay R.D.
dc.contributor.authorEanes R.J.
dc.contributor.authorLemoine F.G.
dc.date.accessioned2021-03-18T00:36:57Z
dc.date.available2021-03-18T00:36:57Z
dc.date.issued2001
dc.description.abstractThe phase lag by which the Earth's body tide follows the tidal potential is estimated for the principal lunar semi-diurnal tide M2. 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 k2, we obtain a lag ε of 0.20°±0.05°, implying an effective body tide Q of 280 and body tide energy dissipation of 110±25 GW.
dc.identifierhttps://www.elibrary.ru/item.asp?id=1205030
dc.identifier.citationGeophysical Journal International, 2001, 144, 2, 471-480
dc.identifier.issn0956-540X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/26872
dc.subjectEARTH TIDES
dc.subjectLOVE NUMBER
dc.subjectOCEAN TIDES
dc.subjectTIDES
dc.titleCONSTRAINTS ON ENERGY DISSIPATION IN THE EARTH'S BODY TIDE FROM SATELLITE TRACKING AND ALTIMETRY
dc.typeСтатья

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