Formula Used:
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Wave Height for Surface Gravity Waves refers to the vertical distance between the trough (bottom) and crest (top) of a wave, measured from sea level. It is calculated using the deepwater wave height, shoaling coefficient, and refraction coefficient.
The calculator uses the formula:
Where:
Explanation: The formula calculates the wave height at a specific location by accounting for shoaling (wave height changes due to varying water depth) and refraction (wave direction changes due to varying water depth).
Details: Accurate wave height calculation is crucial for coastal engineering, navigation safety, beach erosion studies, and offshore structure design. It helps predict wave behavior in shallow water environments.
Tips: Enter wave height in deepwater (m), shoaling coefficient, and refraction coefficient. All values must be positive numbers greater than zero.
Q1: What is shoaling coefficient?
A: Shoaling coefficient is a dimensionless parameter that describes how wave height changes as waves propagate from deep to shallow water due to changes in water depth.
Q2: What is refraction coefficient?
A: Refraction coefficient is a parameter that describes how waves change direction as they propagate from deep water into shallower water near the coastline due to variations in water depth.
Q3: What are typical values for shoaling coefficient?
A: Shoaling coefficient typically ranges from 0.8 to 1.3, depending on water depth and wave characteristics.
Q4: What are typical values for refraction coefficient?
A: Refraction coefficient typically ranges from 0.7 to 1.0, with values closer to 1.0 indicating less wave refraction.
Q5: When is this calculation most important?
A: This calculation is particularly important in coastal areas where waves transition from deep to shallow water, affecting coastal processes and engineering designs.