What is Tide and its detail description ?

  • Earth & Moon exist in isolation
  • Earth is a non rotating sphere
  • A single ocean encircles the globe
  • Ocean is static i.e. has no currents
  • The only forces acting on ocean result from the movement of Earth & Moon about their common center of mass.
Shortcomings of the Equilibrium Model :
  • It predicts semidiurnal tides at all locations – not observed
  • It predicts that high tides should occur when moon passes overhead or 12 hours 25 minutes later – rarely observed
  • Calculations suggest that tidal ranges should be 20-50 cm– observed tidal ranges are often much larger.
  • It predicts values for daily inequities that are rarely observed.
Dynamical Theory of Tides :
  • Begins where equilibrium model ends, i.e. with two bulges created by gravitational interactions of Earth & Moon.
  • Explains real tides by envisioning tidal bulges as tidal wave
  • Tidal wave has small wave height-about 50 cm in open ocean
  • Tidal Wave has a very long wavelength(L) about one half of earth’s circumference = 20,000 kms.
  • Water Depth of oceans = 4 km <<<<< L/2
  • Tidal Wave is a shallow water Wave everywhere, i.e. in interacts continually with the ocean bottom
  • As a shallow water wave, tidal wave feels the bottom, slows, steepens and sometimes breaks
  • Tidal Wave reflects, refracts & interferes with other waves or with reflections of itself
  • Depending upon the shape of a basin, the net result may be a standing wave that corresponds to a diurnal tide, a semidiurnal tide, or a mixed tide.

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