Relative Height of Highest Wave as Function of Wavelength Obtained by Fenton Solution

STEP 0: Pre-Calculation Summary
Formula Used
Relative Height as a function of Wavelength = (0.141063*(Deep-Water Wavelength/Coastal Mean Depth)+0.0095721*(Deep-Water Wavelength/Coastal Mean Depth)^2+0.0077829*(Deep-Water Wavelength/Coastal Mean Depth)^3)/(1+0.078834*(Deep-Water Wavelength/Coastal Mean Depth)+0.0317567*(Deep-Water Wavelength/Coastal Mean Depth)^2+0.0093407*(Deep-Water Wavelength/Coastal Mean Depth)^3)
Hmd = (0.141063*(λo/d)+0.0095721*(λo/d)^2+0.0077829*(λo/d)^3)/(1+0.078834*(λo/d)+0.0317567*(λo/d)^2+0.0093407*(λo/d)^3)
This formula uses 3 Variables
Variables Used
Relative Height as a function of Wavelength - Relative Height as a function of Wavelength refers to the ratio of wave height to wavelength.
Deep-Water Wavelength - (Measured in Meter) - Deep-Water Wavelength is the horizontal distance between two successive crests (or troughs) of the wave.
Coastal Mean Depth - (Measured in Meter) - Coastal Mean Depth of a fluid flow is a measure of the average depth of the fluid in a channel, pipe, or other conduit through which the fluid is flowing.
STEP 1: Convert Input(s) to Base Unit
Deep-Water Wavelength: 7 Meter --> 7 Meter No Conversion Required
Coastal Mean Depth: 10 Meter --> 10 Meter No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
Hmd = (0.141063*(λo/d)+0.0095721*(λo/d)^2+0.0077829*(λo/d)^3)/(1+0.078834*(λo/d)+0.0317567*(λo/d)^2+0.0093407*(λo/d)^3) --> (0.141063*(7/10)+0.0095721*(7/10)^2+0.0077829*(7/10)^3)/(1+0.078834*(7/10)+0.0317567*(7/10)^2+0.0093407*(7/10)^3)
Evaluating ... ...
Hmd = 0.0987980050454994
STEP 3: Convert Result to Output's Unit
0.0987980050454994 --> No Conversion Required
FINAL ANSWER
0.0987980050454994 0.098798 <-- Relative Height as a function of Wavelength
(Calculation completed in 00.004 seconds)

Credits

Creator Image
Created by Mithila Muthamma PA
Coorg Institute of Technology (CIT), Coorg
Mithila Muthamma PA has created this Calculator and 2000+ more calculators!
Verifier Image
Verified by M Naveen
National Institute of Technology (NIT), Warangal
M Naveen has verified this Calculator and 900+ more calculators!

Non Linear Wave Theory Calculators

Wave Height given Ursell Number
​ LaTeX ​ Go Wave Height for Surface Gravity Waves = (Ursell Number*Coastal Mean Depth^3)/Deep-Water Wavelength^2
Second Type of Mean Fluid Speed
​ LaTeX ​ Go Mean Horizontal Fluid Velocity = Fluid Stream Velocity-(Rate of Volume Flow/Coastal Mean Depth)
Wave Speed given First Type of Mean Fluid Speed
​ LaTeX ​ Go Wave Speed = Fluid Stream Velocity-Mean Horizontal Fluid Velocity
First Type of Mean Fluid Speed
​ LaTeX ​ Go Mean Horizontal Fluid Velocity = Fluid Stream Velocity-Wave Speed

Relative Height of Highest Wave as Function of Wavelength Obtained by Fenton Formula

​LaTeX ​Go
Relative Height as a function of Wavelength = (0.141063*(Deep-Water Wavelength/Coastal Mean Depth)+0.0095721*(Deep-Water Wavelength/Coastal Mean Depth)^2+0.0077829*(Deep-Water Wavelength/Coastal Mean Depth)^3)/(1+0.078834*(Deep-Water Wavelength/Coastal Mean Depth)+0.0317567*(Deep-Water Wavelength/Coastal Mean Depth)^2+0.0093407*(Deep-Water Wavelength/Coastal Mean Depth)^3)
Hmd = (0.141063*(λo/d)+0.0095721*(λo/d)^2+0.0077829*(λo/d)^3)/(1+0.078834*(λo/d)+0.0317567*(λo/d)^2+0.0093407*(λo/d)^3)

What are the Main Theories for Steady Waves?

There are two main theories for steady waves – Stokes theory, most suitable for waves which are not very long relative to the water depth; and Cnoidal theory, suitable for the other limit where the waves are much longer than the depth. In addition there is one important numerical method – the Fourier approximation method which solves the problem accurately, and is now widely used in ocean and coastal engineering.

How to Calculate Relative Height of Highest Wave as Function of Wavelength Obtained by Fenton?

Relative Height of Highest Wave as Function of Wavelength Obtained by Fenton calculator uses Relative Height as a function of Wavelength = (0.141063*(Deep-Water Wavelength/Coastal Mean Depth)+0.0095721*(Deep-Water Wavelength/Coastal Mean Depth)^2+0.0077829*(Deep-Water Wavelength/Coastal Mean Depth)^3)/(1+0.078834*(Deep-Water Wavelength/Coastal Mean Depth)+0.0317567*(Deep-Water Wavelength/Coastal Mean Depth)^2+0.0093407*(Deep-Water Wavelength/Coastal Mean Depth)^3) to calculate the Relative Height as a function of Wavelength, The Relative Height of Highest Wave as Function of Wavelength Obtained by Fenton is defined as an empirical expression for the relative height of the highest wave Hm/d as a function of wavelength obtained by Fenton (1990). Relative Height as a function of Wavelength is denoted by Hmd symbol.

How to calculate Relative Height of Highest Wave as Function of Wavelength Obtained by Fenton using this online calculator? To use this online calculator for Relative Height of Highest Wave as Function of Wavelength Obtained by Fenton, enter Deep-Water Wavelength o) & Coastal Mean Depth (d) and hit the calculate button. Here is how the Relative Height of Highest Wave as Function of Wavelength Obtained by Fenton calculation can be explained with given input values -> 0.098798 = (0.141063*(7/10)+0.0095721*(7/10)^2+0.0077829*(7/10)^3)/(1+0.078834*(7/10)+0.0317567*(7/10)^2+0.0093407*(7/10)^3).

FAQ

What is Relative Height of Highest Wave as Function of Wavelength Obtained by Fenton?
The Relative Height of Highest Wave as Function of Wavelength Obtained by Fenton is defined as an empirical expression for the relative height of the highest wave Hm/d as a function of wavelength obtained by Fenton (1990) and is represented as Hmd = (0.141063*(λo/d)+0.0095721*(λo/d)^2+0.0077829*(λo/d)^3)/(1+0.078834*(λo/d)+0.0317567*(λo/d)^2+0.0093407*(λo/d)^3) or Relative Height as a function of Wavelength = (0.141063*(Deep-Water Wavelength/Coastal Mean Depth)+0.0095721*(Deep-Water Wavelength/Coastal Mean Depth)^2+0.0077829*(Deep-Water Wavelength/Coastal Mean Depth)^3)/(1+0.078834*(Deep-Water Wavelength/Coastal Mean Depth)+0.0317567*(Deep-Water Wavelength/Coastal Mean Depth)^2+0.0093407*(Deep-Water Wavelength/Coastal Mean Depth)^3). Deep-Water Wavelength is the horizontal distance between two successive crests (or troughs) of the wave & Coastal Mean Depth of a fluid flow is a measure of the average depth of the fluid in a channel, pipe, or other conduit through which the fluid is flowing.
How to calculate Relative Height of Highest Wave as Function of Wavelength Obtained by Fenton?
The Relative Height of Highest Wave as Function of Wavelength Obtained by Fenton is defined as an empirical expression for the relative height of the highest wave Hm/d as a function of wavelength obtained by Fenton (1990) is calculated using Relative Height as a function of Wavelength = (0.141063*(Deep-Water Wavelength/Coastal Mean Depth)+0.0095721*(Deep-Water Wavelength/Coastal Mean Depth)^2+0.0077829*(Deep-Water Wavelength/Coastal Mean Depth)^3)/(1+0.078834*(Deep-Water Wavelength/Coastal Mean Depth)+0.0317567*(Deep-Water Wavelength/Coastal Mean Depth)^2+0.0093407*(Deep-Water Wavelength/Coastal Mean Depth)^3). To calculate Relative Height of Highest Wave as Function of Wavelength Obtained by Fenton, you need Deep-Water Wavelength o) & Coastal Mean Depth (d). With our tool, you need to enter the respective value for Deep-Water Wavelength & Coastal Mean Depth and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.
Let Others Know
Facebook
Twitter
Reddit
LinkedIn
Email
WhatsApp
Copied!