The POLDER instrument is devoted to global observations of the solar radiat
ion reflected by the earth-atmosphere system. Algorithms of the "Earth Radi
ation Budget and Clouds" processing line implemented at the French Space Ce
nter are applied to ADEOS-POLDER data. First results on derived cloud prope
rties are presented from POLDER level 2 data of 10 November 1996 and level
3 products of June 1997.
A good correlation is observed between the POLDER cloud detection algorithm
and the Dynamical Clustering Method applied to METEOSAT data. The multidir
ectional capability of POLDER appears useful to check schemes of cloud opti
cal thickness retrieval. As expected, a water droplet model is suitable for
liquid water clouds and inadequate for ice clouds. That indirectly validat
es our algorithm of cloud phase recognition. An apparent pressure is derive
d from O-2-absorption measurements and a Rayleigh cloud pressure from polar
ization observations. For overcast conditions, the apparent pressure is lar
ger (by more than 100 hPa) than the Rayleigh pressure chiefly due to the ph
oton penetration effect. For partly cloudy conditions, it can be larger or
weaker depending on the surface reflectivity.
Preliminary comparisons between POLDER and ISCCP monthly mean products outl
ine some differences resulting in part from the original characteristics of
POLDER.