What makes the dynamic theory of tides different from the equilibrium theory?

Answer 1

The equilibrium theory was first developed by Newton stating that there is a bulge of water formed from the gravitational pull from the moon and centrifugal pull from the side opposing the moon. this explains most of the reasoning behind tides, but the main thing that it does not account for is that The equilibrium theory was first developed by Newton stating that there is a bulge of water formed from the gravitational pull from the moon and centrifugal pull from the side opposing the moon. this explains most of the reasoning behind tides, but the main thing that it does not account for is that there are landmasses on earth that the bulge of water cannot move over. The dymanic theory of tides was developed by Laploss, Euler and Brunelli. This was a way to account for the land masses. The dynamic theory states that there are many amphidromic systems around the earth, which are similar in a way to clocks that rotate in a circle. The doldrum is at the center of this circle and rotates to counter clockweise in the northern hemisphere and clockweise in the Southern Hemisphere. The "minute hand" on the clock represents a point of high tide and the 180 degree line straight across that "moving minute hand" is its opposing lowtide. not doldrum node *