For an infinitely long, constant-width estuary, the mean water depth is 20 m, and the tidal elevation at the ocean end can be expressed as η = 2 cos (2π/12.42 * t)where the elevation η is in meters and the time t is in hours. Calculate the maximum tidal current velocity (neglect the viscosity effect).
For an infinitely long, constant-width estuary, the mean water depth is 20 m, and the tidal elevation at the ocean end can be expressed as η = 2 cos (2π/12.42 * t)where the elevation η is in meters and the time t is in hours. Calculate the maximum tidal current velocity (neglect the viscosity effect).
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For an infinitely long, constant-width estuary, the mean water depth is 20 m, and the tidal elevation at the ocean end can be expressed as η = 2 cos (2π/12.42 * t)where the elevation η is in meters and the time t is in hours. Calculate the maximum tidal current velocity (neglect the viscosity effect).
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