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Monday, Nov. 28, 2005 - UTA HEP WWW Home Page
Monday, Nov. 28, 2005 - UTA HEP WWW Home Page

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CHAPTER 3 Methodology and Geophysical Data

... together cause an increase in mean that sea-level gravitational acceleration of about 0.5% from equator to poles. The figure of the Earth is the shape of an equipotentional surface of gravity, in particular the one that coincides with mean sea level, which is called geoid (Li and Gőtze, 2001). The b ...
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Monday, Nov. 28, 2005 - UTA HEP WWW Home Page

... – An area of space where there is no charges or conduction currents – In other words, far from emf sources so that the wave fronts are essentially flat or not distorted over a reasonable area – What are these flat waves called? • Plane waves • At any instance E and B are uniform over a large plane p ...
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Speed of gravity

In classical theories of gravitation, the speed of gravity is the speed at which changes in a gravitational field propagate. This is the speed at which a change in the distribution of energy and momentum of matter results in subsequent alteration, at a distance, of the gravitational field which it produces. In a more physically correct sense, the ""speed of gravity"" refers to the speed of a gravitational wave, which in turn is the same speed as the speed of light (c).
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