Physics
Scientific paper
May 2007
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007agusm.p41b..11h&link_type=abstract
American Geophysical Union, Spring Meeting 2007, abstract #P41B-11
Physics
0343 Planetary Atmospheres (5210, 5405, 5704), 2459 Planetary Ionospheres (5435, 5729, 6026), 3304 Atmospheric Electricity, 3311 Clouds And Aerosols, 6281 Titan
Scientific paper
During the descent of the HUYGENS Probe through the atmosphere of Titan, January 14th, 2005, the Permittivity, Waves and Altimetry (PWA), a subsystem of the HUYGENS Atmospheric Structure Instrument (HASI) detected an ionized layer around the altitude of 60 km with two different instruments, the Relaxation Probe (RP) and the Mutual Impedance Probe (MIP). For both instruments a more detailed data analysis, including unforeseen environmental effects, was necessary to reach precise quantitative estimations of the electrical conductivity. The present work is dedicated to the MIP data analysis. New laboratory tests have been performed to correct and validate the calibration data. Temperature effects have been included and two different numerical models of MIP electrodes and circuits in the HUYGENS body have been used. The effect of motion of HUYGENS in the ionized atmosphere that was neglected in the first analysis is revealed and analytical estimations of this effect allow to derive more accurate values of the conductivity profile. The final results are discussed and compared to the RP results. Electron density profiles are deduced showing more precisely the lower ionized layer and its surprisingly steep lower and higher boundaries, not predicted by any model. We conclude that the spatial variability of the free electron density is probably due to aerosol layers that can capture the electrons created in the medium.
Béghin Christian
Berthelier Jean-Jacques
Brown V. J.
Chabassiere M.
Falkner Peter
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