Publication Date:
2013
abstract:
We have analyzed limb daytime observations of Titan's
upper atmosphere at 3.3 um, acquired by the visual-infrared
mapping spectrometer (VIMS) on Cassini. They were
previously studied by GarcĂa-Comas et al. (2011) to derive
CH4 densities. Here, we report an unidentified emission
peaking around 3.28 um, hidden under the methane
R branch. This emission is very strong, with intensity
comparable to the CH4 bands located in the same spectral
region. It presents a maximum at about 950 km and extends
from 600 km up to 1250 km. It is definitely pumped
by solar radiation since it vanishes at night. Our analysis
shows that neither methane nor the major hydrocarbon
compounds already discovered in Titan's upper atmosphere
are responsible for it. We have discarded many other
potential candidates and suggest that the unidentified
emission might be caused by aromatic compounds.
Iris type:
01.01 Articolo in rivista
List of contributors:
Dinelli, BIANCA MARIA; Moriconi, MARIA LUISA
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