Evapotranspiration (version 1.9)

ET.MortonCRWE: Morton CRWE Formulation

Description

Implementing the Morton CRWE formulation for estimating potential evapotranspiration or shallow lake evaporation.

Usage

## S3 method for class 'MortonCRWE':
ET(data, constants, ts="monthly", est="potential ET", 
solar="sunshine hours", Tdew= T, alpha = NULL, \dots)

Arguments

data

A list of data which contains the following items (climate variables) required by Morton CRWE formulation: Tmax, Tmin, Tdew, Rs or n or Cd

constants

A list named constants consists of constants required for the calculation of Morton CRWE formulation which must contain the following items: Elev - ground elevation above mean sea level in m, lat_rad - latitude in radians, <

ts

Must be either monthly or annual, which indicates the disired time step that the output ET estimates should be on. Default is monthly.

solar

Must be either data, sunshine hours, cloud or monthly precipitation: data indicates that solar radiation data is to be used directly for calculating evapotranspiration; sunshine hours

est

Must be either potential ET or shallow lake ET: potential ET proceeds to estimating potential evapotranspiration; shallow lake ET proceeds to estimating shallow lake evaporation. Default is potenti

Tdew

Must be T or F, indicating if real data of dew point temperature is used for calculating the radiation in Morton's formulations, if T the data will be used and if F the dew point temperature will be calc

alpha

Only needed if argument solar has value of data. Any numeric value between 0 and 1 (dimensionless), albedo of evaporative surface representing the portion of the incident radiation that is reflected back at the surface. Default

...

Dummy for generic function, no need to define.

Value

• The function prints a calculation summary to the screen containign the following elements: - ET model name and ET quantity estimated (i.e. the value of argument est) - Option for calculating solar radiation (i.e. the value of argument solar) - If the actual dew point temperature data are used (i.e. the value of argument Tdew) - Time step of the output ET estimates (i.e. the value of argument ts) - Units of the output ET estimates - Time duration of the ET estimation - Number of ET estimates obtained in the entire time-series - Basic statistics of the estimated ET time-series including mean, max and min values. The function also generates a list containing the following components, which is saved into a csv file named as ET_MortonCRWE.csv in the working directory:
• ET.Daily
  Daily aggregated estimations of MortonCRWE potential evapotranspiration or shallow lake evaporation.
• ET.Monthly
  Monthly aggregated estimations of MortonCRWE potential evapotranspiration or shallow lake evaporation.
• ET.Annual
  Annually aggregated estimations of MortonCRWE potential evapotranspiration or shallow lake evaporation.
• ET.MonthlyAve
  Monthly averaged estimations of daily MortonCRWE potential evapotranspiration or shallow lake evaporation.
• ET.AnnualAve
  Annually averaged estimations of daily MortonCRWE potential evapotranspiration or shallow lake evaporation.
• ET_formulation
  Name of the formulation used which equals to MortonCRWE.
• ET_type
  Type of the estimation obtained which is either Potential Evapotranspiration or Shallow Lake Evaporation.
• message1
  A message to inform the users about how solar radiation has been calculated by using which data.
• message6
  A message to inform the users about if actual dew point temperature has been used in the calculations or alternative calculations has been performed without dew point temperature data.

Details

The type of evapotranspiration calculated can be selected through argument est, please see Arguments for details. The alternative calculation options can be selected through argument solar and Tdew, please see Arguments for details.

References

McMahon, T., Peel, M., Lowe, L., Srikanthan, R. & McVicar, T. 2012. Estimating actual, potential, reference crop and pan evaporation using standard meteorological data: a pragmatic synthesis. Hydrology and Earth System Sciences Discussions, 9, 11829-11910. Morton, F.I. 1983, Operational estimates of lake evaporation. Journal of Hydrology, vol. 66, no. 1-4, pp. 77-100.

See Also

data,defaultconstants,constants,ET.MortonCRWE

Examples

# Use processed existing data set and constants from 
# kent Town, Adelaide
data("processeddata")
data("constants")

# Call ET.MortonCRWE under the generic function ET
results <- ET.MortonCRWE(data, constants, ts="monthly",
est="potential ET", solar="sunshine hours", Tdew= TRUE, 
alpha = NULL)