Cj. Stubenrauch et al., DETERMINATION OF LONGWAVE ANISOTROPIC EMISSION FACTORS FROM COMBINED BROAD-BAND AND NARROW-BAND RADIANCE MEASUREMENTS, Journal of applied meteorology, 32(5), 1993, pp. 848-856
The conversion of measured radiances into radiative fluxes requires ap
plication of angular corrections: in the Earth Radiation Budget Experi
ment (ERBE), the longwave anisotropic emission factors (AEFs) were tab
ulated for different viewing zenith angles, seasons, latitude bands, a
nd scene types, including four different cloud-cover classes. An alter
native approach is investigated using simultaneous infrared atmospheri
c window (10.5-12.5 mum) and broadband longwave (LW) measurements. Suc
h measurements will be available from the ScaRaB (Scanner for Radiatio
n Balance) instrument whose launch is planned to occur in 1993. Using
a radiative transfer model to simulate the combined measurements, the
AEF is parametrized as a function of viewing zenith angle and a single
other variable-atmospheric pseudoabsorptance-defined as the normalize
d difference between the broadband LW radiance and the integrated Plan
ck emission at the 11.5-mum brightness temperature. For validation of
the parameterization with existing satellite data, simultaneous colloc
ated NOAA-9 ERBE Advanced Very High Resolution Radiometer data were us
ed for broad- and narrowband radiances. The comparison between fluxes
corrected with the parameterized AEF and those corrected with the ERBE
AEF shows that the parameterization provides more realistic AEFs as a
function of scene brightness temperature, which is related to cloud-t
op height. Analysis of classified cloud data indicates that there are
only a few extreme cases in which additional anisotropy due to broken
clouds will affect the usefulness of this parameterization. Enhanced a
nisotropy of semitransparent cirrus was also considered. Model and dat
a show that although not explicitly treated in this procedure, the par
ameterization gives good results. This parameterization may also be ad
apted for somewhat different wavelength bands as in the NASA CERES (Cl
ouds and the Earth's Radiant Energy System) project.