Tidal Amplitude in Ocean Calculator

✖Bay Superelevation means that the average level of the bay is greater than the average elevation of the ocean over a given time period.ⓘ Bay Superelevation [Δ_BS]			+10% -10%
✖Duration of Inflow is the period over which a stream or river carries a consistent flow of water into a system.ⓘ Duration of Inflow [t]			+10% -10%
✖Tidal Period is the time taken for a specific site on Earth to rotate from an exact point under moon to same point under moon, also known as “tidal day” and it’s slightly longer than a solar day.ⓘ Tidal Period [T]			+10% -10%

✖Ocean Tide Amplitude is the height difference between high and low tides, reflecting gravitational forces from the moon and sun.ⓘ Tidal Amplitude in Ocean [a_o]

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Download Bay Superelevation, Effect of Freshwater Inflow, Multiple Inlets and Wave Current Interaction Formulas PDF PDF Image

Tidal Amplitude in Ocean Solution

STEP 0: Pre-Calculation Summary

Formula Used

Ocean Tide Amplitude = Bay Superelevation/(sin(2*pi*Duration of Inflow/Tidal Period)/(1-cos(2*pi*Duration of Inflow/Tidal Period)))
a_o = Δ_BS/(sin(2*pi*t/T)/(1-cos(2*pi*t/T)))
This formula uses 1 Constants, 2 Functions, 4 Variables

Constants Used

pi - Archimedes' constant Value Taken As 3.14159265358979323846264338327950288

Functions Used

sin - Sine is a trigonometric function that describes the ratio of the length of the opposite side of a right triangle to the length of the hypotenuse., sin(Angle)
cos - Cosine of an angle is the ratio of the side adjacent to the angle to the hypotenuse of the triangle., cos(Angle)

Variables Used

Ocean Tide Amplitude - (Measured in Meter) - Ocean Tide Amplitude is the height difference between high and low tides, reflecting gravitational forces from the moon and sun.
Bay Superelevation - (Measured in Meter) - Bay Superelevation means that the average level of the bay is greater than the average elevation of the ocean over a given time period.
Duration of Inflow - (Measured in Second) - Duration of Inflow is the period over which a stream or river carries a consistent flow of water into a system.
Tidal Period - (Measured in Second) - Tidal Period is the time taken for a specific site on Earth to rotate from an exact point under moon to same point under moon, also known as “tidal day” and it’s slightly longer than a solar day.

STEP 1: Convert Input(s) to Base Unit

Bay Superelevation: 4.51 Meter --> 4.51 Meter No Conversion Required
Duration of Inflow: 1.2 Hour --> 4320 Second (Check conversion here)
Tidal Period: 130 Second --> 130 Second No Conversion Required

STEP 2: Evaluate Formula

Substituting Input Values in Formula

a_o = Δ_BS/(sin(2*pi*t/T)/(1-cos(2*pi*t/T))) --> 4.51/(sin(2*pi*4320/130)/(1-cos(2*pi*4320/130)))

Evaluating ... ...

a_o = 3.99551134833178

STEP 3: Convert Result to Output's Unit

3.99551134833178 Meter --> No Conversion Required

FINAL ANSWER

3.99551134833178 ≈ 3.995511 Meter <-- Ocean Tide Amplitude

(Calculation completed in 00.004 seconds)

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Home » Engineering » Civil » Coastal and Ocean Engineering » Hydrodynamics of Tidal Inlets 1 » Inlet Hydrodynamics » Bay Superelevation, Effect of Freshwater Inflow, Multiple Inlets and Wave Current Interaction » Bay Superelevation » Tidal Amplitude in Ocean

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Created by Mithila Muthamma PA

Coorg Institute of Technology (CIT), Coorg

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National Institute of Technology (NIT), Warangal

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< Bay Superelevation Calculators

Superelevation due to Varying Entrance Channel Cross-Section

LaTeX Go 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))

Tidal Amplitude in Ocean

LaTeX Go Ocean Tide Amplitude = Bay Superelevation/(sin(2*pi*Duration of Inflow/Tidal Period)/(1-cos(2*pi*Duration of Inflow/Tidal Period)))

Superelevation

LaTeX Go Bay Superelevation = Ocean Tide Amplitude*(sin(2*pi*Duration of Inflow/Tidal Period)/(1-cos(2*pi*Duration of Inflow/Tidal Period)))

Depth given Water Surface Slope

LaTeX Go Eckman Constant Depth = (Coefficient of Eckman*Shear Stress at the Water Surface)/(Water Surface Slope*Water Density*[g])

Tidal Amplitude in Ocean Formula

LaTeX Go

Ocean Tide Amplitude = Bay Superelevation/(sin(2*pi*Duration of Inflow/Tidal Period)/(1-cos(2*pi*Duration of Inflow/Tidal Period)))
a_o = Δ_BS/(sin(2*pi*t/T)/(1-cos(2*pi*t/T)))

What is Bay Superelevation?

A Superelevation of 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. The effect of long-term (months or years) rises in sea level causing a long-term rise in bay level is not included in this definition of bay superelevation, since both sea and bay are responding simultaneously. The bay may not rise at the same rate as the sea due to possible circulation effects if multiple inlets connect the bay to the ocean.

What is Ocean Dynamics & Ocean Tide?

Ocean dynamics define and describe the motion of water within the oceans. Ocean temperature and motion fields can be separated into three distinct layers: mixed (surface) layer, upper ocean (above the thermocline), and deep ocean. Ocean dynamics have traditionally been investigated by sampling from instruments in situ.
Tides are caused by the gravitational pull of the moon and the sun. Tides are very long-period waves that move through the oceans in response to the forces exerted by the moon and sun. Tides originate in the oceans and progress toward the coastlines where they appear as the regular rise and fall of the sea surface.

How to Calculate Tidal Amplitude in Ocean?

Tidal Amplitude in Ocean calculator uses Ocean Tide Amplitude = Bay Superelevation/(sin(2*pi*Duration of Inflow/Tidal Period)/(1-cos(2*pi*Duration of Inflow/Tidal Period))) to calculate the Ocean Tide Amplitude, The Tidal Amplitude in Ocean formula is defined as the elevation of tidal high water above mean sea level. Ocean Tide Amplitude is denoted by a_o symbol.

How to calculate Tidal Amplitude in Ocean using this online calculator? To use this online calculator for Tidal Amplitude in Ocean, enter Bay Superelevation (Δ_BS), Duration of Inflow (t) & Tidal Period (T) and hit the calculate button. Here is how the Tidal Amplitude in Ocean calculation can be explained with given input values -> 3.995511 = 4.51/(sin(2*pi*4320/130)/(1-cos(2*pi*4320/130))).

FAQ

What is Tidal Amplitude in Ocean?

The Tidal Amplitude in Ocean formula is defined as the elevation of tidal high water above mean sea level and is represented as a_o = Δ_BS/(sin(2*pi*t/T)/(1-cos(2*pi*t/T))) or Ocean Tide Amplitude = Bay Superelevation/(sin(2*pi*Duration of Inflow/Tidal Period)/(1-cos(2*pi*Duration of Inflow/Tidal Period))). Bay Superelevation means that the average level of the bay is greater than the average elevation of the ocean over a given time period, Duration of Inflow is the period over which a stream or river carries a consistent flow of water into a system & Tidal Period is the time taken for a specific site on Earth to rotate from an exact point under moon to same point under moon, also known as “tidal day” and it’s slightly longer than a solar day.

How to calculate Tidal Amplitude in Ocean?

The Tidal Amplitude in Ocean formula is defined as the elevation of tidal high water above mean sea level is calculated using Ocean Tide Amplitude = Bay Superelevation/(sin(2*pi*Duration of Inflow/Tidal Period)/(1-cos(2*pi*Duration of Inflow/Tidal Period))). To calculate Tidal Amplitude in Ocean, you need Bay Superelevation (Δ_BS), Duration of Inflow (t) & Tidal Period (T). With our tool, you need to enter the respective value for Bay Superelevation, Duration of Inflow & Tidal Period and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.

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