pt3 | R Documentation |
This function returns the inverse CDF of the Pearson type III distribution, that is, the K value. It is calculated based on the approximation of: Kite (1977), Frequency and Risk Analysis in Hydrology, Water Resouces Publications, Fourt Collins. as cited in: Chow, Maidment, and Mays (1988), Applied Hydrology, ch. 12
pt3(c, Fx)
c |
skewness of sample |
Fx |
non-exceedence probability, F(x)= |
the inverse CDF or K value
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