Several issues remain unresolved, still. There has been so far very little validation of the results; the
accuracy of the retrieved corrected reflectances should be carefully assessed with field and airborne
experiments on selected sites. Whether or not atmospheric corrections should be performed prior to the
application of a bidirectional reflectance model should be debated. A key criterion in this issue is the accuracy
with which atmospheric corrections can be performed. The quality of atmospheric corrections can be expected
to improve in the next decade, with the development of ground based Sun-photometer network (eg, Holben et
al., 1994), General Circulation Models, and satellite data such as those of the POLDER/ADEOS instrument. It
is our personal opinion, still little justified, that this should favor composition methods where atmospheric
corrections are performed as a first step. An other debatable issue concerns the trade-off between the number
of free parameters to be retrieved in the regression process, and the duration of the composition period. Several
compromises have been presented in this paper, without providing conclusive evidence that a solution is by far
better than the others. Finally, inversion of bidirectional reflectance models in terms of other parameters than
the corrected reflectance appears difficult with AVHRR data. This latter conclusion should however be re
examined in the case of future sensors, such as POLDER/ADEOS (Deschamps et al., 1994) or MISR/EOS
(Diner et al., 1989), for which (i) the number of directional data available for each terrestrial target will be
much larger than for AVHRR in a given period of time, (ii) the directional space, in particular in azimuth, will
be much better covered than with AVHRR.
ACKNOWLEDGMENTS
The author thanks M. Ba, F. Cabot, G. Dedieu, P.Y. Deschamps, R. Frouin and J.L. Roujean for providing a
copy of their manuscript prior to publication and allowing the author to comment their results in this paper.
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