ANALYSIS OF TEMPORAL VARIATIONS OF THE POLARIZATION OF VENUS OBSERVEDBY PIONEER VENUS ORBITER

Citation
Wjj. Knibbe et al., ANALYSIS OF TEMPORAL VARIATIONS OF THE POLARIZATION OF VENUS OBSERVEDBY PIONEER VENUS ORBITER, J GEO R-PLA, 103(E4), 1998, pp. 8557-8574
Citations number
50
Categorie Soggetti
Geosciences, Interdisciplinary","Astronomy & Astrophysics","Geochemitry & Geophysics",Oceanografhy,"Metereology & Atmospheric Sciences
Journal title
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
ISSN journal
21699097 → ACNP
Volume
103
Issue
E4
Year of publication
1998
Pages
8557 - 8574
Database
ISI
SICI code
2169-9097(1998)103:E4<8557:AOTVOT>2.0.ZU;2-G
Abstract
Time variations of the disk-averaged polarization of Venus at waveleng ths of 270, 365, 550, and 935 nm have been analyzed in terms of averag e haze optical thickness, cloud-top pressure, and cloud absorption opt ical thickness at 210 nm (presumably due to gaseous SO2 absorption). T he polarization data were deduced from observations made by the Pionee r Venus Orbiter between 1978 and 1990. Newton-Raphson iteration was us ed to derive the atmospheric parameter values from these observations. The required multiple scattering calculations were performed using th e adding/doubling method. The atmospheric model consists of a cloud la yer and a haze layer. The cloud and haze particles are composed of a c oncentrated sulfuric acid solution and have an effective radius of 1.0 5 mu m and 0.25 mu m, respectively. It was found that the disk-average d haze optical thickness, cloud-top pressure, and cloud absorption opt ical thickness at 270 nm varied irregularly between 1978 and 1990. No trends were identified for the cloud-top pressure and cloud absorption optical thickness at 270 nm, but we did deduce a decrease in haze opt ical thickness during this 12 year period. Specific numbers are: (1) a haze optical thickness at 365 nm of about 0.25 in 1978 and less than 0.1 in 1990, (2) a cloud-top pressure that varies between 5 and 20 mba r, and (3) a cloud absorption optical thickness that varies between 0. 0 and 4.0. Finally, our analysis revealed that the disk-averaged cloud -top pressure and haze optical thickness behaved anomalously in 1983.