Bayesian methods are used to develop a cloud mask classification algorithm
for use in an operational sea surface temperature (SST) retrieval processin
g system for Advanced Very High Resolution Radiometer (AVHRR) area coverage
(LAC) resolution data. Both radiative and spatial features are incorporate
d in the resulting discriminant functions, which are determined from a larg
e training sample of cloudy and clear observations. This approach obviates
the need to specify the arbitrary thresholds used by hierarchical cloud-cle
aring methods, provides an estimate of the probability that an instantaneou
s field of view is cloudy (clear), and allows the skill of different cloud
discriminant models to be objectively analyzed.
Results show that spatial information is of particular importance in reduci
ng the false alarm rate of the cloudy class. However, while the use of comp
lex textural measures such as gray-level difference statistics-as opposed t
o simple statistics such as the standard deviation-improves the skill of ni
ghttime cloud-masking algorithms, they are of little advantage during dayti
me hours.
Cloud mask discriminant models having similar high Kuipers' performance ind
ex scores (i.e., 0.935) are developed for both day and night satellite data
from the Southern Hemisphere midlatitudes. Applied to LAC orbital (i.e., o
perational) data, the characteristics of the cloud masks appear to be simil
ar to those derived from analysis of the training sample data. However, in
this case. to enhance processing performance, a hybrid algorithm is employe
d-obviously cloudy instantaneous fields of view (IFOVs) are first removed v
ia a gross Ihreshold check and the Bayesian method applied only to the rema
ining IFOVs. This same (hybrid) algorithm is also applied to an ensemble of
30 days of AVHRR LAC data from the New Zealand region. Analysis of the res
ulting time-composited SST data (means and standard deviations) shows there
is little evidence of a day-night bias in the performance of the Bayesian
cloud-masking algorithm and that the resulting SST data may be used to dete
rmine the variability of oceanographic features.
Although this paper uses AVHRR data to demonstrate the principles of the Ba
yesian cloud-masking algorithm, there is no reason why the approach could n
ot be used with other instruments.