M. Leroy et al., RETRIEVAL OF ATMOSPHERIC PROPERTIES AND SURFACE BIDIRECTIONAL REFLECTANCES OVER LAND FROM POLDER ADEOS/, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 102(D14), 1997, pp. 17023-17037
Polarization and Directionality of the Earth's Reflectances (POLDER) i
s a new instrument devoted to the global observation of the polarizati
on and directionality of solar radiation reflected by the Earth-atmosp
here system It will fly onboard the ADEOS platform in 1996. This paper
outlines the improvements expected from POLDER in the description of
atmospheric aerosols and water vapor over land, and of surface bidirec
tional reflectances. It then gives a detailed description of the opera
tional algorithms which are implemented in the ''land surface and atmo
sphere over land'' processing line. This line is part of an effort ini
tiated by Centre National d'Etudes Spatiales (the French Space Agency)
to develop lines of products in order to facilitate the exploration o
f POLDER's new capabilities by the international science community. Em
phasis is given in this paper to the presentation of the principles, p
hysical rationale, and elements of validation of the algorithms of thi
s processing line. The main products are (1) for each orbit segment, t
he amount and type of aerosols, the water vapor content, and bidirecti
onal reflectances corrected for atmospheric effects, and (2) every 10
days, global maps of surface directional signatures, of hemispherical
surface reflectances, and of parameters describing the statistical dis
tribution of aerosol and water vapor content. These products will be m
ade available to all interested investigators. The most innovative alg
orithms of the processing line are (1) cloud detection, based on a ser
ies of tests involving reflectance thresholds, oxygen pressure estimat
es, and analysis of polarized radiance in the rainbow direction, (2) r
etrieval of aerosol optical thickness and type from directional polari
zed radiance measurements, and (3) retrieval of surface directional si
gnature through an adjustment of a time series of directional reflecta
nce measurements with a semiempirical bidirectional reflectance model.