Formula Used:
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Root Mean Square Wave Height is the square root of the average of the squares of all wave heights. It provides a statistical measure of wave height variability based on the Rayleigh distribution.
The calculator uses the formula:
Where:
Explanation: This formula converts the average wave height to the root mean square wave height using the statistical properties of the Rayleigh distribution.
Details: Root Mean Square Wave Height is crucial for ocean engineering, coastal management, and wave energy studies as it provides a more accurate representation of wave energy and wave-induced forces on structures.
Tips: Enter the average of all waves based on Rayleigh distribution in meters. The value must be greater than zero.
Q1: What is the Rayleigh distribution in wave statistics?
A: The Rayleigh distribution is a statistical model used to describe the distribution of wave heights in a sea state, particularly for narrow-band Gaussian processes.
Q2: How does RMS wave height differ from significant wave height?
A: RMS wave height is the square root of the mean of squared wave heights, while significant wave height is the average of the highest one-third of waves. They are related but represent different statistical measures.
Q3: When is this calculation most applicable?
A: This calculation is most applicable for fully developed sea states where wave heights follow Rayleigh distribution, typically in deep water conditions.
Q4: Are there limitations to this formula?
A: The formula assumes perfect Rayleigh distribution, which may not hold in shallow water, during wave breaking, or in mixed sea states with multiple wave systems.
Q5: What engineering applications use RMS wave height?
A: RMS wave height is used in structural design of offshore platforms, calculation of wave loads on coastal structures, and estimation of wave energy resources.