Superelevation due to Varying Entrance Channel Cross-Section evaluator uses Superelevation = Ocean Tide Amplitude*(1-(((Bay Tide Amplitude/Ocean Tide Amplitude)^2)/(4*(Channel Depth/Ocean Tide Amplitude)))-(Ocean Tide Amplitude/(Bank Slope*Channel Width corresponding to Mean Water Depth))*(0.5-(Bay Tide Amplitude/Ocean Tide Amplitude)*cos(Phase Lag)-((3/2)*(Bay Tide Amplitude/Ocean Tide Amplitude)^2)+4*(Channel Depth/Ocean Tide Amplitude)^2)) to evaluate the Superelevation, The Superelevation due to Varying Entrance Channel Cross-Section formula is defined as the bay means that the average level of the bay is greater than the average elevation of the ocean over a given time period. An obvious cause of this effect is the introduction of freshwater into the bay from local rivers and streams. Superelevation is denoted by S symbol.
How to evaluate Superelevation due to Varying Entrance Channel Cross-Section using this online evaluator? To use this online evaluator for Superelevation due to Varying Entrance Channel Cross-Section, enter Ocean Tide Amplitude (ao), Bay Tide Amplitude (aB), Channel Depth (Dt), Bank Slope (m), Channel Width corresponding to Mean Water Depth (W) & Phase Lag (k) and hit the calculate button.