The aim of this work is to deduce physical characteristics of the aerosols
that compose the thin detached haze layer of Titan, for which the compositi
on and origin are currently unknown. We have used four images at three diff
erent phase angles and three different wavelengths where the detached haze
clearly appears. The low optical path in the layer permits assumptions that
greatly simplify the treatment and allow us to consider the scattered inte
nsity as the product of the scattering cross section, the phase function at
the considered phase angle, and the number of aerosols, Physical arguments
are given to support fractal aerosols in the detached haze, and we investi
gate a wide range of monomer radii, monomer numbers, and imaginary refracti
ve indexes. This study yields information about the spectral variation of t
he refractive index for the detached haze tholins that are clearly differen
t from those for the main haze. On the other hand, no firm values are given
for the monomer radius and number, but these two parameters are strongly l
inked through a simple relation. (C) 2000 Academic Press.