MadSci Network: Earth Sciences |
The long term change in Earth's rotation is caused mainly by the "breaking" of the Earth due to tidal friction. As our planet deforms continuosly by the effect of the attraction of the Sun and the Moon (and all the other bodies, in fact), the water in the ocean (and all other water masses) flows in the bottom, and the dissipated energy changes the rotation rate of the planet, by the conservation of angular momentum. By this process, we have an increase in the length of the day by 2.3 milliseconds per century nowadays. The fossil register indicates that some 370 million years ago the day had 22 hours. Only with the extended capabilities of measuring the daily variations in the rotation rate in recent years we could account for minor (or rapid) effects, such as the diurnal and semidiurnal variations. There are two main causes for these variations, the movement of water around the globe by the tides, that changes the moment of inertia of the earth, and the tidal velocity variations, that exchange angular momentum with the solid earth. So, the increase in population and the damming of rivers can be classified in the diurnal and semidiurnal variations, although it should be stressed that the involved masses in this case are very small and the effect should be small if compared with the other effects. Information about tides can be found in the web pages of Special Bureau for Tides (http://bowie.gsfc.nasa.gov/ggfc/tides/tides.html). Some good references: Munk, W. H. 'Once again: once again--tidal friction', Progress in Oceanography, vol. 40, pp. 7-36, 1997. Munk, W. H. and G. J. F. MacDonald, The Rotation of the Earth: A Geophysical Discussion, Cambridge Univ. Press, 1960. Lambeck, K., The Earth's Variable Rotation: Geophysical Causes and Consequences, Cambridge Univ. Press, 1980. Best regards Eder C. Molina (eder@iag.usp.br) Geophysicist Dept. of Geophysics Institute of Astronomy, Geophysics and Atmospheric Sciences University of Sao Paulo BRAZIL
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