Horizontal Component of Local Fluid Velocity Calculator

✖Height of the Wave is the difference between the elevations of a crest and a neighboring trough.ⓘ Height of the Wave [H_w]			+10% -10%
✖Wave Period refers to the time it takes for two successive wave crests (or troughs) to pass through a given point.ⓘ Wave Period [T_p]			+10% -10%
✖Wavelength of Wave refers to the distance between consecutive corresponding points of the same phase on the wave, such as two adjacent crests, troughs, or zero crossings.ⓘ Wavelength of Wave [λ]			+10% -10%
✖Distance above the Bottom refers to the vertical measurement from the lowest point of a given surface (such as the bottom of waterbody) to a specified point above it.ⓘ Distance above the Bottom [D_Z+d]			+10% -10%
✖Water Depth for Fluid Velocity is the depth as measured from the water level to the bottom of the considered water body.ⓘ Water Depth for Fluid Velocity [d]			+10% -10%
✖Phase Angle refers to the time lag between the maximum amplitude of a forcing function, such as waves or currents, and the response of the system, such as water level or sediment transport.ⓘ Phase Angle [θ]			+10% -10%

✖Horizontal Component of Velocity is the speed of water movement parallel to the shoreline. It's a crucial parameter in understanding coastal dynamics and plays a significant role in coastal processes.ⓘ Horizontal Component of Local Fluid Velocity [H_v]

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Horizontal Component of Local Fluid Velocity Solution

STEP 0: Pre-Calculation Summary

Formula Used

Horizontal Component of Velocity = (Height of the Wave*[g]*Wave Period/(2*Wavelength of Wave))*((cosh((2*pi*Distance above the Bottom)/Wavelength of Wave))/(cosh((2*pi*Water Depth for Fluid Velocity)/Wavelength of Wave)))*cos(Phase Angle)
H_v = (H_w*[g]*T_p/(2*λ))*((cosh((2*pi*D_Z+d)/λ))/(cosh((2*pi*d)/λ)))*cos(θ)
This formula uses 2 Constants, 2 Functions, 7 Variables

Constants Used

[g] - Gravitational acceleration on Earth Value Taken As 9.80665
pi - Archimedes' constant Value Taken As 3.14159265358979323846264338327950288

Functions Used

cos - Cosine of an angle is the ratio of the side adjacent to the angle to the hypotenuse of the triangle., cos(Angle)
cosh - The hyperbolic cosine function is a mathematical function that is defined as the ratio of the sum of the exponential functions of x and negative x to 2., cosh(Number)

Variables Used

Horizontal Component of Velocity - (Measured in Meter per Second) - Horizontal Component of Velocity is the speed of water movement parallel to the shoreline. It's a crucial parameter in understanding coastal dynamics and plays a significant role in coastal processes.
Height of the Wave - (Measured in Meter) - Height of the Wave is the difference between the elevations of a crest and a neighboring trough.
Wave Period - (Measured in Second) - Wave Period refers to the time it takes for two successive wave crests (or troughs) to pass through a given point.
Wavelength of Wave - (Measured in Meter) - Wavelength of Wave refers to the distance between consecutive corresponding points of the same phase on the wave, such as two adjacent crests, troughs, or zero crossings.
Distance above the Bottom - (Measured in Meter) - Distance above the Bottom refers to the vertical measurement from the lowest point of a given surface (such as the bottom of waterbody) to a specified point above it.
Water Depth for Fluid Velocity - (Measured in Meter) - Water Depth for Fluid Velocity is the depth as measured from the water level to the bottom of the considered water body.
Phase Angle - (Measured in Radian) - Phase Angle refers to the time lag between the maximum amplitude of a forcing function, such as waves or currents, and the response of the system, such as water level or sediment transport.

STEP 1: Convert Input(s) to Base Unit

Height of the Wave: 14 Meter --> 14 Meter No Conversion Required
Wave Period: 95 Second --> 95 Second No Conversion Required
Wavelength of Wave: 32 Meter --> 32 Meter No Conversion Required
Distance above the Bottom: 2 Meter --> 2 Meter No Conversion Required
Water Depth for Fluid Velocity: 17 Meter --> 17 Meter No Conversion Required
Phase Angle: 30 Degree --> 0.5235987755982 Radian (Check conversion here)

STEP 2: Evaluate Formula

Substituting Input Values in Formula

H_v = (H_w*[g]*T_p/(2*λ))*((cosh((2*pi*D_Z+d)/λ))/(cosh((2*pi*d)/λ)))*cos(θ) --> (14*[g]*95/(2*32))*((cosh((2*pi*2)/32))/(cosh((2*pi*17)/32)))*cos(0.5235987755982)

Evaluating ... ...

H_v = 13.4963328458748

STEP 3: Convert Result to Output's Unit

13.4963328458748 Meter per Second --> No Conversion Required

FINAL ANSWER

13.4963328458748 ≈ 13.49633 Meter per Second <-- Horizontal Component of Velocity

(Calculation completed in 00.020 seconds)

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Home » Engineering » Civil » Coastal and Ocean Engineering » Water Wave Mechanics » Local Fluid and Mass Transport Velocity » Local Fluid Velocity » Horizontal Component of Local Fluid Velocity

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Coorg Institute of Technology (CIT), Coorg

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< Local Fluid Velocity Calculators

Local Fluid Particle Acceleration of Vertical Component of Fluid Velocity

LaTeX Go Local Fluid Particle Acceleration in Y Direction = -([g]*pi*Height of the Wave/Wavelength of Wave)*((sinh(2*pi*(Distance above the Bottom)/Wavelength of Wave))/(cosh(2*pi*Water Depth for Fluid Velocity/Wavelength of Wave)))*cos(Phase Angle)

Local Fluid Particle Acceleration of Horizontal Component

LaTeX Go Local Fluid Particle Acceleration in X Direction = ([g]*pi*Height of the Wave/Wavelength of Wave)*((cosh(2*pi*(Distance above the Bottom)/Wavelength of Wave))/(cosh(2*pi*Water Depth for Fluid Velocity/Wavelength of Wave)))*sin(Phase Angle)

Horizontal Component of Local Fluid Velocity

LaTeX Go Horizontal Component of Velocity = (Height of the Wave*[g]*Wave Period/(2*Wavelength of Wave))*((cosh((2*pi*Distance above the Bottom)/Wavelength of Wave))/(cosh((2*pi*Water Depth for Fluid Velocity)/Wavelength of Wave)))*cos(Phase Angle)

Vertical Component of Local Fluid Velocity

LaTeX Go Vertical Component of Velocity = (Height of the Wave*[g]*Wave Period/(2*Wavelength of Wave))*((sinh(2*pi*(Distance above the Bottom)/Wavelength of Wave))/(cosh(2*pi*Water Depth for Fluid Velocity/Wavelength of Wave)))*sin(Phase Angle)

Horizontal Component of Local Fluid Velocity Formula

LaTeX Go

How Does Depth Affect Wavelength?

The change from deep to shallow water waves occurs when the depth of the water, d, becomes less than one half of the wavelength of the wave, λ. The speed of deep-water waves depends on the wavelength of the waves. We say that deep-water waves show dispersion. A wave with a longer wavelength travels at higher speed.

How to Calculate Horizontal Component of Local Fluid Velocity?

Horizontal Component of Local Fluid Velocity calculator uses Horizontal Component of Velocity = (Height of the Wave*[g]*Wave Period/(2*Wavelength of Wave))*((cosh((2*pi*Distance above the Bottom)/Wavelength of Wave))/(cosh((2*pi*Water Depth for Fluid Velocity)/Wavelength of Wave)))*cos(Phase Angle) to calculate the Horizontal Component of Velocity, The Horizontal Component of Local Fluid Velocity formula is defined as the speed and direction of water movement parallel to the shoreline at a specific point. Horizontal Component of Velocity is denoted by H_v symbol.

How to calculate Horizontal Component of Local Fluid Velocity using this online calculator? To use this online calculator for Horizontal Component of Local Fluid Velocity, enter Height of the Wave (H_w), Wave Period (T_p), Wavelength of Wave (λ), Distance above the Bottom (D_Z+d), Water Depth for Fluid Velocity (d) & Phase Angle (θ) and hit the calculate button. Here is how the Horizontal Component of Local Fluid Velocity calculation can be explained with given input values -> 13.49633 = (14*[g]*95/(2*32))*((cosh((2*pi*2)/32))/(cosh((2*pi*17)/32)))*cos(0.5235987755982).

FAQ

What is Horizontal Component of Local Fluid Velocity?

The Horizontal Component of Local Fluid Velocity formula is defined as the speed and direction of water movement parallel to the shoreline at a specific point and is represented as H_v = (H_w*[g]*T_p/(2*λ))*((cosh((2*pi*D_Z+d)/λ))/(cosh((2*pi*d)/λ)))*cos(θ) or Horizontal Component of Velocity = (Height of the Wave*[g]*Wave Period/(2*Wavelength of Wave))*((cosh((2*pi*Distance above the Bottom)/Wavelength of Wave))/(cosh((2*pi*Water Depth for Fluid Velocity)/Wavelength of Wave)))*cos(Phase Angle). Height of the Wave is the difference between the elevations of a crest and a neighboring trough, Wave Period refers to the time it takes for two successive wave crests (or troughs) to pass through a given point, Wavelength of Wave refers to the distance between consecutive corresponding points of the same phase on the wave, such as two adjacent crests, troughs, or zero crossings, Distance above the Bottom refers to the vertical measurement from the lowest point of a given surface (such as the bottom of waterbody) to a specified point above it, Water Depth for Fluid Velocity is the depth as measured from the water level to the bottom of the considered water body & Phase Angle refers to the time lag between the maximum amplitude of a forcing function, such as waves or currents, and the response of the system, such as water level or sediment transport.

How to calculate Horizontal Component of Local Fluid Velocity?

The Horizontal Component of Local Fluid Velocity formula is defined as the speed and direction of water movement parallel to the shoreline at a specific point is calculated using Horizontal Component of Velocity = (Height of the Wave*[g]*Wave Period/(2*Wavelength of Wave))*((cosh((2*pi*Distance above the Bottom)/Wavelength of Wave))/(cosh((2*pi*Water Depth for Fluid Velocity)/Wavelength of Wave)))*cos(Phase Angle). To calculate Horizontal Component of Local Fluid Velocity, you need Height of the Wave (H_w), Wave Period (T_p), Wavelength of Wave (λ), Distance above the Bottom (D_Z+d), Water Depth for Fluid Velocity (d) & Phase Angle (θ). With our tool, you need to enter the respective value for Height of the Wave, Wave Period, Wavelength of Wave, Distance above the Bottom, Water Depth for Fluid Velocity & Phase Angle 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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