Root Mean Square Wave Height Formula:
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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 energy based on the Rayleigh distribution assumption for wave heights.
The calculator uses the Rayleigh distribution formula:
Where:
Explanation: Under the Rayleigh distribution assumption for wave heights, the significant wave height (mean of highest 1/3 waves) is approximately 1.414 times the root mean square wave height.
Details: RMS wave height is crucial for wave energy calculations, coastal engineering design, and understanding wave statistics in oceanography. It provides a more stable statistical measure than individual wave heights.
Tips: Enter significant wave height in meters. The value must be positive and valid for accurate RMS wave height calculation.
Q1: What is the relationship between Hs and Hrms?
A: Under Rayleigh distribution, significant wave height (Hs) is approximately 1.414 times the root mean square wave height (Hrms).
Q2: When is the Rayleigh distribution assumption valid?
A: The Rayleigh distribution is a good approximation for fully developed sea states with narrow-banded wave spectra.
Q3: What are typical values for Hrms?
A: Hrms values vary widely depending on sea conditions, from less than 0.5m in calm seas to over 10m in extreme storm conditions.
Q4: How accurate is this conversion?
A: The conversion is mathematically exact under the Rayleigh distribution assumption, but real ocean waves may deviate from this ideal distribution.
Q5: What engineering applications use Hrms?
A: Hrms is used in wave energy calculations, coastal structure design, sediment transport studies, and offshore operations planning.