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The top documents tagged [tidal current amplitude]
Typical Mean Dynamic Balances in Estuaries Along-Estuary Component 1. Barotropic pressure gradient vs. friction Steady state, linear motion, no rotation,
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The Open Shelf Sea. 1. The primary source of buoyancy is surface heat flux. c p = specific heat capacity of seawater (= 3900 J kg -1 K -1 ) mean water
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Temporal Variability Tidal Subtidal Wind and Atmospheric Pressure Fortnightly
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