On Tidal Energy Horizontal Circulation

  • Nekrasov, A.V. (Physical Oceanography, Russian State Hydrometeorological Institute)
  • 발행 : 1992.08.01

초록

The local horizintal flux of tidal energy is characterized by the surface density $\omega$ = $\rho$ g h ζ u ($\rho$ - sea water density, g - gravitation, h - depth, ζ - tidal surface elevation, u - vertically averaged tidal current velocity vector). In general the flux vector $\omega$ comprises active and reactive components whose relation determines the local structure of a tidal wave.(omitted)

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