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Estimates the cloudiness of the atmosphere by scaling to atmospheric transmissivity
EstCloudiness(Tx=(-999), Tn=(-999), trans=NULL, transMin = 0.15, transMax = 0.75, opt = "linear")
maximum daily temperature [C]
minimum daily temperature [C]
transmissivity of the atmosphere (value between 0-1)
Transmissivities equal and below this value will return a cloudiness value of 1 (for linear approximation)
Transmissivities equal and above this value will return a cloudiness value of 0 (for linear approximation)
Currently there are two options: "linear" (Campbell 1985) and "Black" (1956)
Campbell G.S. (1985) Soil Physics with Basic: Transport Models for Soil Plant Systems. Elsevier, New York
Black, J.N. (1956) The Distribution of Solar Radiation over the Earth's Surface. Theoretical and Applied Climatology 7:2 165-189
# NOT RUN { EstCloudiness(trans=0.2) EstCloudiness(20,12,opt="Black") # }
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