Parameter Including Wind Velocity and Saturation Deficit Calculator

✖Daily Potential Evapotranspiration is the process by which water is transferred from the land to the atmosphere by evaporation from the soil and other surfaces and by transpiration from plants.ⓘ Daily Potential Evapotranspiration [PET]			+10% -10%
✖Slope of Saturation Vapour Pressure vs temperature curve at the mean air temperature, in mm of mercury per °C.ⓘ Slope of Saturation Vapour Pressure [A]			+10% -10%
✖Psychrometric Constant relates the partial pressure of water in air to the air temperature.ⓘ Psychrometric Constant [γ]			+10% -10%
✖Net Radiation of Evaporable Water length per day influenced by the incoming solar radiation absorbed by the Earth's surface and the radiation reflected back.ⓘ Net Radiation of Evaporable Water [H_n]			+10% -10%

✖Parameter of Wind Velocity and Saturation Deficit.ⓘ Parameter Including Wind Velocity and Saturation Deficit [E_a]

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Parameter Including Wind Velocity and Saturation Deficit Solution

STEP 0: Pre-Calculation Summary

Formula Used

Parameter of Wind Velocity and Saturation Deficit = (Daily Potential Evapotranspiration*(Slope of Saturation Vapour Pressure+Psychrometric Constant)-(Slope of Saturation Vapour Pressure*Net Radiation of Evaporable Water))/Psychrometric Constant
E_a = (PET*(A+γ)-(A*H_n))/γ
This formula uses 5 Variables

Variables Used

Parameter of Wind Velocity and Saturation Deficit - Parameter of Wind Velocity and Saturation Deficit.
Daily Potential Evapotranspiration - Daily Potential Evapotranspiration is the process by which water is transferred from the land to the atmosphere by evaporation from the soil and other surfaces and by transpiration from plants.
Slope of Saturation Vapour Pressure - Slope of Saturation Vapour Pressure vs temperature curve at the mean air temperature, in mm of mercury per °C.
Psychrometric Constant - Psychrometric Constant relates the partial pressure of water in air to the air temperature.
Net Radiation of Evaporable Water - Net Radiation of Evaporable Water length per day influenced by the incoming solar radiation absorbed by the Earth's surface and the radiation reflected back.

STEP 1: Convert Input(s) to Base Unit

Daily Potential Evapotranspiration: 2.06 --> No Conversion Required
Slope of Saturation Vapour Pressure: 1.05 --> No Conversion Required
Psychrometric Constant: 0.49 --> No Conversion Required
Net Radiation of Evaporable Water: 1.99 --> No Conversion Required

STEP 2: Evaluate Formula

Substituting Input Values in Formula

E_a = (PET*(A+γ)-(A*H_n))/γ --> (2.06*(1.05+0.49)-(1.05*1.99))/0.49

Evaluating ... ...

E_a = 2.21

STEP 3: Convert Result to Output's Unit

2.21 --> No Conversion Required

FINAL ANSWER

2.21 <-- Parameter of Wind Velocity and Saturation Deficit

(Calculation completed in 00.004 seconds)

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< Evapotranspiration Equations Calculators

Mean Monthly Air Temperature for Potential Evapotranspiration in Thornthwaite Equation

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LaTeX Go Adjustment Factor = Potential Evapotranspiration in Crop Season/(1.6*((10*Mean Air Temperature)/Total Heat Index)^An Empirical Constant)

Thornthwaite Formula

LaTeX Go Potential Evapotranspiration in Crop Season = 1.6*Adjustment Factor*((10*Mean Air Temperature)/Total Heat Index)^An Empirical Constant

Equation for Blaney Criddle

LaTeX Go Potential Evapotranspiration in Crop Season = 2.54*An Empirical Coefficient*Sum of Monthly Consumptive Use factors

Parameter Including Wind Velocity and Saturation Deficit Formula

LaTeX Go

What causes Wind Velocity?

The Wind is caused by differences in atmospheric pressure. When a difference in atmospheric pressure exists, air moves from the higher to the lower pressure area, resulting in winds of various speeds or Wind Velocity.

How to Calculate Parameter Including Wind Velocity and Saturation Deficit?

Parameter Including Wind Velocity and Saturation Deficit calculator uses Parameter of Wind Velocity and Saturation Deficit = (Daily Potential Evapotranspiration*(Slope of Saturation Vapour Pressure+Psychrometric Constant)-(Slope of Saturation Vapour Pressure*Net Radiation of Evaporable Water))/Psychrometric Constant to calculate the Parameter of Wind Velocity and Saturation Deficit, The Parameter Including Wind Velocity and Saturation Deficit formula is defined as the amount by which the water vapour in the air must be increased to achieve saturation without changing the environmental temperature and pressure. Parameter of Wind Velocity and Saturation Deficit is denoted by E_a symbol.

How to calculate Parameter Including Wind Velocity and Saturation Deficit using this online calculator? To use this online calculator for Parameter Including Wind Velocity and Saturation Deficit, enter Daily Potential Evapotranspiration (PET), Slope of Saturation Vapour Pressure (A), Psychrometric Constant (γ) & Net Radiation of Evaporable Water (H_n) and hit the calculate button. Here is how the Parameter Including Wind Velocity and Saturation Deficit calculation can be explained with given input values -> 2.21 = (2.06*(1.05+0.49)-(1.05*1.99))/0.49.

FAQ

What is Parameter Including Wind Velocity and Saturation Deficit?

The Parameter Including Wind Velocity and Saturation Deficit formula is defined as the amount by which the water vapour in the air must be increased to achieve saturation without changing the environmental temperature and pressure and is represented as E_a = (PET*(A+γ)-(A*H_n))/γ or Parameter of Wind Velocity and Saturation Deficit = (Daily Potential Evapotranspiration*(Slope of Saturation Vapour Pressure+Psychrometric Constant)-(Slope of Saturation Vapour Pressure*Net Radiation of Evaporable Water))/Psychrometric Constant. Daily Potential Evapotranspiration is the process by which water is transferred from the land to the atmosphere by evaporation from the soil and other surfaces and by transpiration from plants, Slope of Saturation Vapour Pressure vs temperature curve at the mean air temperature, in mm of mercury per °C, Psychrometric Constant relates the partial pressure of water in air to the air temperature & Net Radiation of Evaporable Water length per day influenced by the incoming solar radiation absorbed by the Earth's surface and the radiation reflected back.

How to calculate Parameter Including Wind Velocity and Saturation Deficit?

The Parameter Including Wind Velocity and Saturation Deficit formula is defined as the amount by which the water vapour in the air must be increased to achieve saturation without changing the environmental temperature and pressure is calculated using Parameter of Wind Velocity and Saturation Deficit = (Daily Potential Evapotranspiration*(Slope of Saturation Vapour Pressure+Psychrometric Constant)-(Slope of Saturation Vapour Pressure*Net Radiation of Evaporable Water))/Psychrometric Constant. To calculate Parameter Including Wind Velocity and Saturation Deficit, you need Daily Potential Evapotranspiration (PET), Slope of Saturation Vapour Pressure (A), Psychrometric Constant (γ) & Net Radiation of Evaporable Water (H_n). With our tool, you need to enter the respective value for Daily Potential Evapotranspiration, Slope of Saturation Vapour Pressure, Psychrometric Constant & Net Radiation of Evaporable Water 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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