Wind effects on a rain gauge can cause a significant underestimation of rai
nfall depths and contribute to the inconsistency in rainfall data. To recon
struct rainfall data requires a consistent method to quantify the undercatc
h. Although some empirical adjustment factors have been recommended, they a
re not generalized enough to reflect the variations of wind speed with resp
ect to height. This paper presents a model by which the undercatch at an el
evated rain gauge can be estimated by the logarithmic wind velocity profile
and raindrop terminal velocity. Deficiency percentages of rain catch predi
cted by this model agree with field observations and recommended adjustment
factors. This approach was further expanded to predict rain undercatch per
centage due to vegetal coverage or other obstructions.