Superelevation evaluator uses Bay Superelevation = Ocean Tide Amplitude*(sin(2*pi*Duration of Inflow/Tidal Period)/(1-cos(2*pi*Duration of Inflow/Tidal Period))) to evaluate the Bay Superelevation, The Superelevation 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. Bay Superelevation is denoted by ΔBS symbol.
How to evaluate Superelevation using this online evaluator? To use this online evaluator for Superelevation, enter Ocean Tide Amplitude (ao), Duration of Inflow (t) & Tidal Period (T) and hit the calculate button.