L. Digirolamo et R. Davies, CLOUD FRACTION ERRORS CAUSED BY FINITE RESOLUTION MEASUREMENTS, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 102(D2), 1997, pp. 1739-1756
The standard method of deriving cloud fraction from space simply finds
the fraction of total image pixels that contains some cloud. The sens
itivity of this method to sensor resolution has been examined by Shenk
and Salomonson [1972], assuming the cloudy pixels are detected perfec
tly. Their experiment is reexamined to show that the sensitivity is mu
ch more complex than they predicted. We derive the upper and lower bou
nds of the true cloud fraction, A(t), given the standard method estima
te, A(e), to show that the range of possible values for A(t) can be, i
n general, very wide. By including the fraction of apparent cloud edge
and cloud interior pixels, the bounds can be reduced and improvements
to the standard method can be obtained. However, this improvement is
also resolution limited by the misidentification of partially cloudy p
ixels as cloud interior rather than cloud edge. A potentially better t
echnique for estimating the true cloud fraction is therefore explored
using a pattern recognition approach. A nearest neighbor classificatio
n rule is used in two sets of experiments: one using 684 simulated clo
ud fields as a training set, the other using 370 cloud fields based on
Advanced Very High Resolution Radiometer (AVHRR) measurements. Given
the underlying distribution of A(t), A(e) overestimates A(t) with an o
verall average bias of 32% and standard error of 11% for the simulated
training set, and a bias of 35% and a standard error of 3% for the AV
HRR training set. The pattern recognition estimate, A(p), is essential
ly unbiased and has a standard error of 12% for both training sets. Th
e relevance of these training sets to new scenes and the importance of
imperfect cloud detection have yet to be investigated, but the patter
n recognition technique shows considerable potential advantage over th
e standard technique in providing unbiased estimates of cloud fraction
that are less sensitive to the effects of sensor resolution.