Friction Velocity of Wind in Neutral Stratification as Function of Geostrophic Wind Speed Solution

STEP 0: Pre-Calculation Summary
Formula Used
Friction Velocity = 0.0275*Geostrophic Wind Speed
Vf = 0.0275*Ug
This formula uses 2 Variables
Variables Used
Friction Velocity - (Measured in Meter per Second) - Friction velocity, also called Shear velocity, is a form by which a shear stress may be re-written in units of velocity.
Geostrophic Wind Speed - (Measured in Meter per Second) - Geostrophic Wind Speed s a theoretical wind speed that results from a balance between the Coriolis force and the pressure-gradient force, concepts explored in greater detail in later readings.
STEP 1: Convert Input(s) to Base Unit
Geostrophic Wind Speed: 9.99 Meter per Second --> 9.99 Meter per Second No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
Vf = 0.0275*Ug --> 0.0275*9.99
Evaluating ... ...
Vf = 0.274725
STEP 3: Convert Result to Output's Unit
0.274725 Meter per Second --> No Conversion Required
FINAL ANSWER
0.274725 Meter per Second <-- Friction Velocity
(Calculation completed in 00.004 seconds)

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24 Estimating Marine and Coastal Winds Calculators

Wind Speed at Height above Surface in form of near Surface Wind Profile
​ Go Wind Speed = (Friction Velocity/Von Kármán Constant)*(ln(Height z above Surface/Roughness Height of Surface)-Universal Similarity Function*(Height z above Surface/Parameter with Dimensions of Length))
Coefficient of Drag for Winds Influenced by Stability Effects given Von Karman Constant
​ Go Coefficient of Drag = (Von Kármán Constant/(ln(Height z above Surface/Roughness Height of Surface)-Universal Similarity Function*(Height z above Surface/Parameter with Dimensions of Length)))^2
Gradient of Atmospheric Pressure Orthogonal to Isobars given Gradient Wind Speed
​ Go Gradient of Atmospheric Pressure = (Gradient Wind Speed-(Gradient Wind Speed^2/(Coriolis Frequency*Radius of Curvature of Isobars)))/(1/(Density of Air*Coriolis Frequency))
Friction Velocity given Wind Speed at Height above Surface
​ Go Friction Velocity = Von Kármán Constant*(Wind Speed/(ln(Height z above Surface/Roughness Height of Surface)))
Wind Speed at Height z above Surface
​ Go Wind Speed = (Friction Velocity/Von Kármán Constant)*ln(Height z above Surface/Roughness Height of Surface)
Wind Stress in Parametric Form
​ Go Wind Stress = Coefficient of Drag*(Density of Air/Water Density)*Wind Speed^2
Friction Velocity given Wind Stress
​ Go Friction Velocity = sqrt(Wind Stress/(Density of Air/Water Density))
Gradient of Atmospheric Pressure Orthogonal to Isobars
​ Go Gradient of Atmospheric Pressure = Geostrophic Wind Speed/(1/(Density of Air*Coriolis Frequency))
Geostrophic Wind Speed
​ Go Geostrophic Wind Speed = (1/(Density of Air*Coriolis Frequency))*Gradient of Atmospheric Pressure
Friction Velocity given Height of Boundary Layer in Non-Equatorial Regions
​ Go Friction Velocity = (Height of Boundary Layer*Coriolis Frequency)/Dimensionless Constant
Height of Boundary layer in Non-Equatorial Regions
​ Go Height of Boundary Layer = Dimensionless Constant*(Friction Velocity/Coriolis Frequency)
Wind Speed given Coefficient of Drag at 10-m Reference Level
​ Go Wind Speed = sqrt(Wind Stress/Coefficient of Drag to 10m Reference Level)
Wind Stress given Friction Velocity
​ Go Wind Stress = (Density of Air/Water Density)*Friction Velocity^2
Wind Speed at Height z above Surface given Standard Reference Wind Speed
​ Go Wind Speed = Wind Speed at Height of 10 m/(10/Height z above Surface)^(1/7)
Wind Speed at Standard 10-m Reference Level
​ Go Wind Speed at Height of 10 m = Wind Speed*(10/Height z above Surface)^(1/7)
Height z above Surface given Standard Reference Wind Speed
​ Go Height z above Surface = 10/(Wind Speed at Height of 10 m/Wind Speed)^7
Rate of Momentum Transfer at Standard Reference Height for Winds
​ Go Wind Stress = Coefficient of Drag to 10m Reference Level*Wind Speed^2
Coefficient of Drag at 10m Reference Level given Wind Stress
​ Go Coefficient of Drag to 10m Reference Level = Wind Stress/Wind Speed^2
Air-Sea Temperature Difference
​ Go Air-Sea Temperature Difference = (Air Temperature-Water Temperature)
Water Temperature given Air-Sea Temperature Difference
​ Go Water Temperature = Air Temperature-Air-Sea Temperature Difference
Air Temperature given Air-Sea Temperature Difference
​ Go Air Temperature = Air-Sea Temperature Difference+Water Temperature
Coefficient of Drag for Winds Influenced by Stability Effects
​ Go Coefficient of Drag = (Friction Velocity/Wind Speed)^2
Friction Velocity of Wind in Neutral Stratification as Function of Geostrophic Wind Speed
​ Go Friction Velocity = 0.0275*Geostrophic Wind Speed
Geostrophic Wind Speed given Friction Velocity in Neutral Stratification
​ Go Geostrophic Wind Speed = Friction Velocity/0.0275

Friction Velocity of Wind in Neutral Stratification as Function of Geostrophic Wind Speed Formula

Friction Velocity = 0.0275*Geostrophic Wind Speed
Vf = 0.0275*Ug

What is Friction Velocity?

Shear velocity, also called friction velocity, is a form by which shear stress may be rewritten in units of velocity. It is useful as a method in fluid mechanics to compare true velocities, such as the velocity of a flow in a stream, to a velocity that relates shear between layers of flow.

What is Geostrophic Wind?

The Geostrophic wind is a theoretical wind speed that results from a balance between the Coriolis force and the pressure-gradient force, concepts explored in greater detail in later readings.

How to Calculate Friction Velocity of Wind in Neutral Stratification as Function of Geostrophic Wind Speed?

Friction Velocity of Wind in Neutral Stratification as Function of Geostrophic Wind Speed calculator uses Friction Velocity = 0.0275*Geostrophic Wind Speed to calculate the Friction Velocity, The Friction Velocity of Wind in Neutral Stratification as Function of Geostrophic Wind Speed formula is defined as the form by which shear stress may be re-written in units of velocity. Friction Velocity is denoted by Vf symbol.

How to calculate Friction Velocity of Wind in Neutral Stratification as Function of Geostrophic Wind Speed using this online calculator? To use this online calculator for Friction Velocity of Wind in Neutral Stratification as Function of Geostrophic Wind Speed, enter Geostrophic Wind Speed (Ug) and hit the calculate button. Here is how the Friction Velocity of Wind in Neutral Stratification as Function of Geostrophic Wind Speed calculation can be explained with given input values -> 0.274725 = 0.0275*9.99.

FAQ

What is Friction Velocity of Wind in Neutral Stratification as Function of Geostrophic Wind Speed?
The Friction Velocity of Wind in Neutral Stratification as Function of Geostrophic Wind Speed formula is defined as the form by which shear stress may be re-written in units of velocity and is represented as Vf = 0.0275*Ug or Friction Velocity = 0.0275*Geostrophic Wind Speed. Geostrophic Wind Speed s a theoretical wind speed that results from a balance between the Coriolis force and the pressure-gradient force, concepts explored in greater detail in later readings.
How to calculate Friction Velocity of Wind in Neutral Stratification as Function of Geostrophic Wind Speed?
The Friction Velocity of Wind in Neutral Stratification as Function of Geostrophic Wind Speed formula is defined as the form by which shear stress may be re-written in units of velocity is calculated using Friction Velocity = 0.0275*Geostrophic Wind Speed. To calculate Friction Velocity of Wind in Neutral Stratification as Function of Geostrophic Wind Speed, you need Geostrophic Wind Speed (Ug). With our tool, you need to enter the respective value for Geostrophic Wind Speed and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.
How many ways are there to calculate Friction Velocity?
In this formula, Friction Velocity uses Geostrophic Wind Speed. We can use 3 other way(s) to calculate the same, which is/are as follows -
  • Friction Velocity = Von Kármán Constant*(Wind Speed/(ln(Height z above Surface/Roughness Height of Surface)))
  • Friction Velocity = sqrt(Wind Stress/(Density of Air/Water Density))
  • Friction Velocity = (Height of Boundary Layer*Coriolis Frequency)/Dimensionless Constant
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