<P> Newton, in the Principia, provided a correct explanation for the tidal force, which can be used to explain tides on a planet covered by a uniform ocean, but which takes no account of the distribution of the continents or ocean bathymetry . </P> <P> The dynamic theory of tides describes and predicts the actual real behavior of ocean tides . </P> <P> While Newton explained the tides by describing the tide - generating forces and Bernoulli gave a description of the static reaction of the waters on Earth to the tidal potential, the dynamic theory of tides, developed by Pierre - Simon Laplace in 1775, describes the ocean's real reaction to tidal forces . Laplace's theory of ocean tides took into account friction, resonance and natural periods of ocean basins . It predicted the large amphidromic systems in the world's ocean basins and explains the oceanic tides that are actually observed . The equilibrium theory, based on the gravitational gradient from the Sun and Moon but ignoring the Earth's rotation, the effects of continents, and other important effects, could not explain the real ocean tides . Since measurements have confirmed the theory, many things have possible explanations now, like how the tides interact with deep sea ridges and chains of seamounts give rise to deep eddies that transport nutrients from the deep to the surface . The equilibrium tide theory calculates the height of the tide wave of less than half a meter, while the dynamic theory explains why tides are up to 15 meters . Satellite observations confirm the accuracy of the dynamic theory, and the tides worldwide are now measured to within a few centimeters . Measurements from the CHAMP satellite closely match the models based on the TOPEX data . Accurate models of tides worldwide are essential for research since the variations due to tides must be removed from measurements when calculating gravity and changes in sea levels . </P> <Table> <Tr> <Td> A. Lunar gravitational potential: this depicts the Moon directly over 30 ° N (or 30 ° S) viewed from above the Northern Hemisphere . </Td> <Td> B . This view shows same potential from 180 ° from view A. Viewed from above the Northern Hemisphere . Red up, blue down . </Td> </Tr> </Table>

Who had propounded the dynamic theory of origin of ocean tides