Horizontal Component of Local Fluid Velocity Formula

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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. Check FAQs
Hv=(Hw[g]Tp2λ)(cosh(2πDZ+dλ)cosh(2πdλ))cos(θ)
Hv - Horizontal Component of Velocity?Hw - Height of the Wave?Tp - Wave Period?λ - Wavelength of Wave?DZ+d - Distance above the Bottom?d - Water Depth for Fluid Velocity?θ - Phase Angle?[g] - Gravitational acceleration on Earth?π - Archimedes' constant?

Horizontal Component of Local Fluid Velocity Example

With values
With units
Only example

Here is how the Horizontal Component of Local Fluid Velocity equation looks like with Values.

Here is how the Horizontal Component of Local Fluid Velocity equation looks like with Units.

Here is how the Horizontal Component of Local Fluid Velocity equation looks like.

13.4963Edit=(14Edit9.806695Edit232Edit)(cosh(23.14162Edit32Edit)cosh(23.141617Edit32Edit))cos(30Edit)
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Horizontal Component of Local Fluid Velocity Solution

Follow our step by step solution on how to calculate Horizontal Component of Local Fluid Velocity?

FIRST Step Consider the formula
Hv=(Hw[g]Tp2λ)(cosh(2πDZ+dλ)cosh(2πdλ))cos(θ)
Next Step Substitute values of Variables
Hv=(14m[g]95s232m)(cosh(2π2m32m)cosh(2π17m32m))cos(30°)
Next Step Substitute values of Constants
Hv=(14m9.8066m/s²95s232m)(cosh(23.14162m32m)cosh(23.141617m32m))cos(30°)
Next Step Convert Units
Hv=(14m9.8066m/s²95s232m)(cosh(23.14162m32m)cosh(23.141617m32m))cos(0.5236rad)
Next Step Prepare to Evaluate
Hv=(149.806695232)(cosh(23.1416232)cosh(23.14161732))cos(0.5236)
Next Step Evaluate
Hv=13.4963328458748m/s
LAST Step Rounding Answer
Hv=13.4963m/s

Horizontal Component of Local Fluid Velocity Formula Elements

Variables
Constants
Functions
Horizontal Component of Velocity
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.
Symbol: Hv
Measurement: SpeedUnit: m/s
Note: Value should be greater than 0.
Height of the Wave
Height of the Wave is the difference between the elevations of a crest and a neighboring trough.
Symbol: Hw
Measurement: LengthUnit: m
Note: Value can be positive or negative.
Wave Period
Wave Period refers to the time it takes for two successive wave crests (or troughs) to pass through a given point.
Symbol: Tp
Measurement: TimeUnit: s
Note: Value should be greater than 0.
Wavelength of Wave
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.
Symbol: λ
Measurement: LengthUnit: m
Note: Value can be positive or negative.
Distance above the Bottom
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.
Symbol: DZ+d
Measurement: LengthUnit: m
Note: Value can be positive or negative.
Water Depth for Fluid Velocity
Water Depth for Fluid Velocity is the depth as measured from the water level to the bottom of the considered water body.
Symbol: d
Measurement: LengthUnit: m
Note: Value should be greater than 0.
Phase Angle
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.
Symbol: θ
Measurement: AngleUnit: °
Note: Value can be positive or negative.
Gravitational acceleration on Earth
Gravitational acceleration on Earth means that the velocity of an object in free fall will increase by 9.8 m/s2 every second.
Symbol: [g]
Value: 9.80665 m/s²
Archimedes' constant
Archimedes' constant is a mathematical constant that represents the ratio of the circumference of a circle to its diameter.
Symbol: π
Value: 3.14159265358979323846264338327950288
cos
Cosine of an angle is the ratio of the side adjacent to the angle to the hypotenuse of the triangle.
Syntax: 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.
Syntax: cosh(Number)

Other formulas in Local Fluid Velocity category

​Go Vertical Component of Local Fluid Velocity
Vv=(Hw[g]Tp2λ)(sinh(2πDZ+dλ)cosh(2πdλ))sin(θ)
​Go Local Fluid Particle Acceleration of Horizontal Component
ax=([g]πHwλ)(cosh(2πDZ+dλ)cosh(2πdλ))sin(θ)

How to Evaluate Horizontal Component of Local Fluid Velocity?

Horizontal Component of Local Fluid Velocity evaluator 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 evaluate 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 Hv symbol.

How to evaluate Horizontal Component of Local Fluid Velocity using this online evaluator? To use this online evaluator for Horizontal Component of Local Fluid Velocity, enter Height of the Wave (Hw), Wave Period (Tp), Wavelength of Wave (λ), Distance above the Bottom (DZ+d), Water Depth for Fluid Velocity (d) & Phase Angle (θ) and hit the calculate button.

FAQs on Horizontal Component of Local Fluid Velocity

What is the formula to find Horizontal Component of Local Fluid Velocity?
The formula of Horizontal Component of Local Fluid Velocity is expressed as 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). Here is an example- 13.49633 = (14*[g]*95/(2*32))*((cosh((2*pi*2)/32))/(cosh((2*pi*17)/32)))*cos(0.5235987755982).
How to calculate Horizontal Component of Local Fluid Velocity?
With Height of the Wave (Hw), Wave Period (Tp), Wavelength of Wave (λ), Distance above the Bottom (DZ+d), Water Depth for Fluid Velocity (d) & Phase Angle (θ) we can find Horizontal Component of Local Fluid Velocity using the formula - 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). This formula also uses Gravitational acceleration on Earth, Archimedes' constant and , Cosine (cos), Hyperbolic Cosine (cosh) function(s).
Can the Horizontal Component of Local Fluid Velocity be negative?
No, the Horizontal Component of Local Fluid Velocity, measured in Speed cannot be negative.
Which unit is used to measure Horizontal Component of Local Fluid Velocity?
Horizontal Component of Local Fluid Velocity is usually measured using the Meter per Second[m/s] for Speed. Meter per Minute[m/s], Meter per Hour[m/s], Kilometer per Hour[m/s] are the few other units in which Horizontal Component of Local Fluid Velocity can be measured.
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