Wave Height Formula:
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Wave Height of a surface wave is the difference between the elevations of a crest and a neighbouring trough. It's a fundamental parameter in oceanography and coastal engineering that describes the vertical distance between the wave crest and the adjacent wave trough.
The calculator uses the wave height formula:
Where:
Explanation: The formula calculates wave height based on radiation stress component, water density, gravitational acceleration, and wave crest angle using trigonometric functions.
Details: Accurate wave height estimation is crucial for coastal engineering, navigation safety, offshore operations, and understanding coastal processes and sediment transport.
Tips: Enter radiation stress component in N/m, mass density in kg/m³, and wave crest angle in radians. All values must be positive and valid for accurate results.
Q1: What is radiation stress component?
A: Radiation Stress Component is the momentum transferred through the water body per unit of time by wave orbital motion.
Q2: Why is wave crest angle important?
A: Wave crest angle determines how wave energy is distributed and affects wave transformation processes near shorelines.
Q3: What are typical wave height values?
A: Wave heights vary from centimeters (ripples) to over 30 meters (extreme storm waves) depending on wind conditions and fetch.
Q4: How does water density affect wave height?
A: Higher density water requires more energy to create the same wave height, making density a crucial factor in the calculation.
Q5: Are there limitations to this equation?
A: This formula works best for linear wave theory conditions and may need adjustments for extreme waves or complex bathymetry.