Coefficient of Drag at 10m Reference Level given Wind Stress Solution

STEP 0: Pre-Calculation Summary
Formula Used
Coefficient of Drag to 10m Reference Level = Wind Stress/Wind Speed^2
CDZ = τo/U^2
This formula uses 3 Variables
Variables Used
Coefficient of Drag to 10m Reference Level - Coefficient of Drag to 10m Reference Level is used to quantify the drag or resistance of an object in a fluid environment, such as air or water.
Wind Stress - (Measured in Pascal) - Wind Stress is the shear stress exerted by the wind on the surface of large bodies of water.
Wind Speed - (Measured in Meter per Second) - Wind Speed is a fundamental atmospheric quantity caused by air moving from high to low pressure, usually due to changes in temperature.
STEP 1: Convert Input(s) to Base Unit
Wind Stress: 1.5 Pascal --> 1.5 Pascal No Conversion Required
Wind Speed: 4 Meter per Second --> 4 Meter per Second No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
CDZ = τo/U^2 --> 1.5/4^2
Evaluating ... ...
CDZ = 0.09375
STEP 3: Convert Result to Output's Unit
0.09375 --> No Conversion Required
FINAL ANSWER
0.09375 <-- Coefficient of Drag to 10m Reference Level
(Calculation completed in 00.004 seconds)

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Coorg Institute of Technology (CIT), Coorg
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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

Coefficient of Drag at 10m Reference Level given Wind Stress Formula

Coefficient of Drag to 10m Reference Level = Wind Stress/Wind Speed^2
CDZ = τo/U^2

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.

What is 10m Wind?

Surface wind is the wind blowing near the Earth's surface. The wind 10m chart displays the modelled average wind vector 10 m above the ground for every grid point of the model (ca. every 80 km). Generally, the actually observed wind velocity at 10 m above ground is a little bit lower than the modelled one.

How to Calculate Coefficient of Drag at 10m Reference Level given Wind Stress?

Coefficient of Drag at 10m Reference Level given Wind Stress calculator uses Coefficient of Drag to 10m Reference Level = Wind Stress/Wind Speed^2 to calculate the Coefficient of Drag to 10m Reference Level, The Coefficient of Drag at 10m Reference Level given Wind Stress formula is defined as a dimensionless quantity used to quantify an object's drag or resistance in a fluid environment, such as air or water. Coefficient of Drag to 10m Reference Level is denoted by CDZ symbol.

How to calculate Coefficient of Drag at 10m Reference Level given Wind Stress using this online calculator? To use this online calculator for Coefficient of Drag at 10m Reference Level given Wind Stress, enter Wind Stress o) & Wind Speed (U) and hit the calculate button. Here is how the Coefficient of Drag at 10m Reference Level given Wind Stress calculation can be explained with given input values -> 0.09375 = 1.5/4^2.

FAQ

What is Coefficient of Drag at 10m Reference Level given Wind Stress?
The Coefficient of Drag at 10m Reference Level given Wind Stress formula is defined as a dimensionless quantity used to quantify an object's drag or resistance in a fluid environment, such as air or water and is represented as CDZ = τo/U^2 or Coefficient of Drag to 10m Reference Level = Wind Stress/Wind Speed^2. Wind Stress is the shear stress exerted by the wind on the surface of large bodies of water & Wind Speed is a fundamental atmospheric quantity caused by air moving from high to low pressure, usually due to changes in temperature.
How to calculate Coefficient of Drag at 10m Reference Level given Wind Stress?
The Coefficient of Drag at 10m Reference Level given Wind Stress formula is defined as a dimensionless quantity used to quantify an object's drag or resistance in a fluid environment, such as air or water is calculated using Coefficient of Drag to 10m Reference Level = Wind Stress/Wind Speed^2. To calculate Coefficient of Drag at 10m Reference Level given Wind Stress, you need Wind Stress o) & Wind Speed (U). With our tool, you need to enter the respective value for Wind Stress & Wind Speed and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.
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