Adjustment related to Latitude of Place given Potential Evapotranspiration Solution

STEP 0: Pre-Calculation Summary
Formula Used
Adjustment Factor = Potential Evapotranspiration in Crop Season/(1.6*((10*Mean Air Temperature)/Total Heat Index)^An Empirical Constant)
La = ET/(1.6*((10*Ta)/It)^aTh)
This formula uses 5 Variables
Variables Used
Adjustment Factor - Adjustment Factor for the number of hours of daylight and days, in the month, related to the latitude of the place.
Potential Evapotranspiration in Crop Season - (Measured in Centimeter) - Potential Evapotranspiration in Crop Season is the potential evaporation from soils plus transpiration by plants.
Mean Air Temperature - Mean Air Temperature observed for incident solar radiation outside the atmosphere.
Total Heat Index - Total Heat Index Values of a total of twelve months.
An Empirical Constant - An Empirical Constant used in the Thornthwaite Formula depends on the total of 12 monthly values index.
STEP 1: Convert Input(s) to Base Unit
Potential Evapotranspiration in Crop Season: 26.85 Centimeter --> 26.85 Centimeter No Conversion Required
Mean Air Temperature: 20 --> No Conversion Required
Total Heat Index: 10 --> No Conversion Required
An Empirical Constant: 0.93 --> No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
La = ET/(1.6*((10*Ta)/It)^aTh) --> 26.85/(1.6*((10*20)/10)^0.93)
Evaluating ... ...
La = 1.03482380685594
STEP 3: Convert Result to Output's Unit
1.03482380685594 --> No Conversion Required
FINAL ANSWER
1.03482380685594 1.034824 <-- Adjustment Factor
(Calculation completed in 00.004 seconds)

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8 Evapotranspiration Equations Calculators

Equation for Net Radiation of Evaporable Water
Go Net Radiation of Evaporable Water = Incident Solar Radiation Outside the Atmosphere*(1-Reflection Coefficient)*(Constant depending on Latitude+(A constant*Actual Duration of Bright Sunshine/Maximum Possible Hours of Bright Sunshine))-Stefan-Boltzmann constant*Mean Air Temperature^4*(0.56-0.092*sqrt(Actual Vapour Pressure))*(0.1+(0.9*Actual Duration of Bright Sunshine/Maximum Possible Hours of Bright Sunshine))
Net Radiation of Evaporable water given Daily Potential Evapotranspiration
Go Net Radiation of Evaporable Water = (Daily Potential Evapotranspiration*(Slope of Saturation Vapour Pressure+Psychrometric Constant)-(Parameter of Wind Velocity and Saturation Deficit*Psychrometric Constant))/Slope of Saturation Vapour Pressure
Parameter Including Wind Velocity and Saturation Deficit
Go 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
Penman's Equation
Go Daily Potential Evapotranspiration = (Slope of Saturation Vapour Pressure*Net Radiation of Evaporable Water+Parameter of Wind Velocity and Saturation Deficit*Psychrometric Constant)/(Slope of Saturation Vapour Pressure+Psychrometric Constant)
Mean Monthly Air Temperature for Potential Evapotranspiration in Thornthwaite Equation
Go Mean Air Temperature = (Potential Evapotranspiration in Crop Season/(1.6*Adjustment Factor))^(1/An Empirical Constant)*(Total Heat Index/10)
Adjustment related to Latitude of Place given Potential Evapotranspiration
Go Adjustment Factor = Potential Evapotranspiration in Crop Season/(1.6*((10*Mean Air Temperature)/Total Heat Index)^An Empirical Constant)
Thornthwaite Formula
Go Potential Evapotranspiration in Crop Season = 1.6*Adjustment Factor*((10*Mean Air Temperature)/Total Heat Index)^An Empirical Constant
Equation for Blaney Criddle
Go Potential Evapotranspiration in Crop Season = 2.54*An Empirical Coefficient*Sum of Monthly Consumptive Use factors

Adjustment related to Latitude of Place given Potential Evapotranspiration Formula

Adjustment Factor = Potential Evapotranspiration in Crop Season/(1.6*((10*Mean Air Temperature)/Total Heat Index)^An Empirical Constant)
La = ET/(1.6*((10*Ta)/It)^aTh)

What is Potential Evapotranspiration?

Potential evapotranspiration is the potential evaporation from soils plus transpiration by plants. It only occurs at the potential rate when the water available for this process is non-limiting

How to Calculate Adjustment related to Latitude of Place given Potential Evapotranspiration?

Adjustment related to Latitude of Place given Potential Evapotranspiration calculator uses Adjustment Factor = Potential Evapotranspiration in Crop Season/(1.6*((10*Mean Air Temperature)/Total Heat Index)^An Empirical Constant) to calculate the Adjustment Factor, The Adjustment related to Latitude of Place given Potential Evapotranspiration formula is defined as the adjustment factor La for Thornthwaite Equation. Adjustment Factor is denoted by La symbol.

How to calculate Adjustment related to Latitude of Place given Potential Evapotranspiration using this online calculator? To use this online calculator for Adjustment related to Latitude of Place given Potential Evapotranspiration, enter Potential Evapotranspiration in Crop Season (ET), Mean Air Temperature (Ta), Total Heat Index (It) & An Empirical Constant (aTh) and hit the calculate button. Here is how the Adjustment related to Latitude of Place given Potential Evapotranspiration calculation can be explained with given input values -> 1.034824 = 0.2685/(1.6*((10*20)/10)^0.93).

FAQ

What is Adjustment related to Latitude of Place given Potential Evapotranspiration?
The Adjustment related to Latitude of Place given Potential Evapotranspiration formula is defined as the adjustment factor La for Thornthwaite Equation and is represented as La = ET/(1.6*((10*Ta)/It)^aTh) or Adjustment Factor = Potential Evapotranspiration in Crop Season/(1.6*((10*Mean Air Temperature)/Total Heat Index)^An Empirical Constant). Potential Evapotranspiration in Crop Season is the potential evaporation from soils plus transpiration by plants, Mean Air Temperature observed for incident solar radiation outside the atmosphere, Total Heat Index Values of a total of twelve months & An Empirical Constant used in the Thornthwaite Formula depends on the total of 12 monthly values index.
How to calculate Adjustment related to Latitude of Place given Potential Evapotranspiration?
The Adjustment related to Latitude of Place given Potential Evapotranspiration formula is defined as the adjustment factor La for Thornthwaite Equation is calculated using Adjustment Factor = Potential Evapotranspiration in Crop Season/(1.6*((10*Mean Air Temperature)/Total Heat Index)^An Empirical Constant). To calculate Adjustment related to Latitude of Place given Potential Evapotranspiration, you need Potential Evapotranspiration in Crop Season (ET), Mean Air Temperature (Ta), Total Heat Index (It) & An Empirical Constant (aTh). With our tool, you need to enter the respective value for Potential Evapotranspiration in Crop Season, Mean Air Temperature, Total Heat Index & An Empirical Constant 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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