Water Temperature given Air-Sea Temperature Difference Solution

STEP 0: Pre-Calculation Summary
Formula Used
Water Temperature = Air Temperature-Air-Sea Temperature Difference
Ts = Ta-ΔT
This formula uses 3 Variables
Variables Used
Water Temperature - (Measured in Kelvin) - Water Temperature is a physical property expressing how hot or cold water is.
Air Temperature - (Measured in Kelvin) - Air Temperature is a measure of how hot or cold the air is.
Air-Sea Temperature Difference - (Measured in Kelvin) - Air-Sea Temperature Difference of the region under consideration, evaporation is greater with lower humidity in the air, increasing the temperature difference.
STEP 1: Convert Input(s) to Base Unit
Air Temperature: 303 Kelvin --> 303 Kelvin No Conversion Required
Air-Sea Temperature Difference: 55 Kelvin --> 55 Kelvin No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
Ts = Ta-ΔT --> 303-55
Evaluating ... ...
Ts = 248
STEP 3: Convert Result to Output's Unit
248 Kelvin --> No Conversion Required
FINAL ANSWER
248 Kelvin <-- Water Temperature
(Calculation completed in 00.020 seconds)

Credits

Created by Mithila Muthamma PA
Coorg Institute of Technology (CIT), Coorg
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National Institute of Technology (NIT), Warangal
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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

Water Temperature given Air-Sea Temperature Difference Formula

Water Temperature = Air Temperature-Air-Sea Temperature Difference
Ts = Ta-ΔT

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 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 Water Temperature given Air-Sea Temperature Difference?

Water Temperature given Air-Sea Temperature Difference calculator uses Water Temperature = Air Temperature-Air-Sea Temperature Difference to calculate the Water Temperature, The Water Temperature given Air-Sea Temperature Difference formula is defined as a physical property expressing how hot or cold water is. As hot and cold are both arbitrary terms, the temperature can further be defined as a measurement of the average thermal energy of a substance. Water Temperature is denoted by Ts symbol.

How to calculate Water Temperature given Air-Sea Temperature Difference using this online calculator? To use this online calculator for Water Temperature given Air-Sea Temperature Difference, enter Air Temperature (Ta) & Air-Sea Temperature Difference (ΔT) and hit the calculate button. Here is how the Water Temperature given Air-Sea Temperature Difference calculation can be explained with given input values -> 248 = 303-55.

FAQ

What is Water Temperature given Air-Sea Temperature Difference?
The Water Temperature given Air-Sea Temperature Difference formula is defined as a physical property expressing how hot or cold water is. As hot and cold are both arbitrary terms, the temperature can further be defined as a measurement of the average thermal energy of a substance and is represented as Ts = Ta-ΔT or Water Temperature = Air Temperature-Air-Sea Temperature Difference. Air Temperature is a measure of how hot or cold the air is & Air-Sea Temperature Difference of the region under consideration, evaporation is greater with lower humidity in the air, increasing the temperature difference.
How to calculate Water Temperature given Air-Sea Temperature Difference?
The Water Temperature given Air-Sea Temperature Difference formula is defined as a physical property expressing how hot or cold water is. As hot and cold are both arbitrary terms, the temperature can further be defined as a measurement of the average thermal energy of a substance is calculated using Water Temperature = Air Temperature-Air-Sea Temperature Difference. To calculate Water Temperature given Air-Sea Temperature Difference, you need Air Temperature (Ta) & Air-Sea Temperature Difference (ΔT). With our tool, you need to enter the respective value for Air Temperature & Air-Sea Temperature Difference 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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