Friction Velocity Formula:
| From: | To: |
Friction Velocity, also called shear velocity, is a form by which a shear stress may be re-written in units of velocity. It's a fundamental parameter in boundary-layer meteorology used to calculate fluxes of momentum, heat and moisture from the atmosphere to the land surface.
The calculator uses the Friction Velocity formula:
Where:
Explanation: The formula calculates the friction velocity based on wind speed measurements at a specific height above a surface with given roughness characteristics.
Details: Friction velocity is crucial for understanding turbulent transport processes in the atmospheric boundary layer, predicting weather patterns, and modeling air pollution dispersion.
Tips: Enter Von Kármán Constant (typically 0.4), Wind Speed in m/s, Height above Surface in meters, and Roughness Height in meters. All values must be positive and Height must be greater than Roughness Height.
Q1: What is the typical value of Von Kármán Constant?
A: The Von Kármán Constant is typically taken as 0.4 in atmospheric science applications.
Q2: How does surface roughness affect friction velocity?
A: Rougher surfaces (higher z₀) generally result in higher friction velocities for the same wind speed, as more momentum is transferred to the surface.
Q3: What are typical roughness height values?
A: Roughness height varies from ~0.0002 m for smooth water to 1-2 m for forests and urban areas.
Q4: At what height should wind speed be measured?
A: Typically measured at 10 m height for standard meteorological applications, but can vary based on specific requirements.
Q5: What are the limitations of this formula?
A: The formula assumes neutral atmospheric stability and may need adjustments for stable or unstable conditions.