Standing Wave Height Formula:
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Standing Wave Height of Ocean results when two equal waves are going in opposite direction, creating a stationary wave pattern with nodes and antinodes.
The calculator uses the standing wave height formula:
Where:
Explanation: The formula calculates the wave height based on the maximum horizontal velocity at a node and the water depth, using gravitational acceleration as a constant.
Details: Accurate standing wave height calculation is crucial for coastal engineering, harbor design, offshore structure analysis, and understanding wave behavior in confined water bodies.
Tips: Enter maximum horizontal velocity in m/s and water depth in meters. All values must be positive and valid.
Q1: What causes standing waves in oceans?
A: Standing waves occur when two waves of equal frequency and amplitude travel in opposite directions and interfere with each other.
Q2: Where are standing waves commonly observed?
A: In harbors, bays, between breakwaters, and in other confined water bodies where wave reflection occurs.
Q3: What is the significance of nodes in standing waves?
A: Nodes are points where the wave amplitude is minimal, while antinodes are points of maximum amplitude.
Q4: How does water depth affect standing wave height?
A: Deeper water generally allows for larger wave heights, as the relationship is governed by the square root of the depth ratio.
Q5: Are there limitations to this calculation?
A: This formula assumes ideal conditions and may need adjustments for real-world scenarios with complex bathymetry and wave interactions.