Physics
Scientific paper
Mar 1975
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1975natur.254..314b&link_type=abstract
Nature, vol. 254, Mar. 27, 1975, p. 314, 315.
Physics
Anelasticity, Earth Planetary Structure, Earth Rotation, Earth Tides, Earth-Moon System, Phase Error, Crustal Fractures, Earth Crust, Earth Movements, Energy Dissipation, Mechanical Properties, Plastic Deformation, Secular Variations, Tectonics
Scientific paper
The investigation is related to the question whether the bodily tides or ocean tides in the earth-moon system produce most of the energy dissipation which is necessary to account for the secular retardation of the rate of rotation of the earth. In principle a phase lag of about 2 deg of bodily tides, which is enough to account for the whole change, could be obtained from earth tide observations. The results of the investigation indicate that all of the phase lag derived from earth tide observations may be instrumental in origin.
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