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Diurnal variation of electron density in Saturn’s ionosphere: Model comparisons with Saturn Electrostatic Discharge (SED) observations
DOI: 10.1016/j.icarus.2012.08.010 Bibcode: 2012Icar..221..508M

Galand, Marina; Moore, Luke; Fischer, Georg +2 more

Using the Saturn Thermosphere Ionosphere Model (STIM), we present a study of the diurnal variation of electron density, with a focus on comparisons with peak electron densities (NMAX) inferred from the low-frequency cutoff of radio emission due to lightning in the lower atmosphere, called Saturn Electrostatic Discharges (SEDs). It is de…

2012 Icarus
Cassini 9
Cassini-UVIS observation of dayglow FUV emissions of carbon in the thermosphere of Venus
DOI: 10.1016/j.icarus.2012.06.002 Bibcode: 2012Icar..220..635H

Gérard, J. -C.; Hubert, B.; Gladstone, G. R. +3 more

We analyze FUV spatially-resolved dayglow spectra obtained at 0.37 nm resolution by the UVIS instrument during the Cassini flyby of Venus. The intensities of the ultraviolet multiplets of carbon at 126.1, 156.1 and 165.7 nm are determined using a least squares fit technique applied to all dayglow spectra recorded by UVIS along the Cassini track. T…

2012 Icarus
Cassini 9
First ever in situ observations of Venus' polar upper atmosphere density using the tracking data of the Venus Express Atmospheric Drag Experiment (VExADE)
DOI: 10.1016/j.icarus.2011.06.019 Bibcode: 2012Icar..217..831R

Rosenblatt, P.; Häusler, B.; Svedhem, H. +3 more

On its highly elliptical 24 h orbit around Venus, the Venus Express (VEX) spacecraft briefly reaches a periapsis altitude of nominally 250 km. Recently, however, dedicated and intense radio tracking campaigns have taken place in August 2008, October 2009, February and April 2010, for which the periapsis altitude was lowered to the 186-176 km altit…

2012 Icarus
VenusExpress 9
Spatial correlation of OH Meinel and O 2 infrared atmospheric nightglow emissions observed with VIRTIS-M on board Venus Express
DOI: 10.1016/j.icarus.2011.09.010 Bibcode: 2012Icar..217..813G

Drossart, P.; Piccioni, G.; Gérard, J. -C. +1 more

We present the two-dimensional distribution of the O 2 a 1Δ-X 3Σ (0-0) band at 1.27 µm and the OH Δ v = 1 Meinel airglow measured simultaneously with the Visible and Infrared Thermal Imaging Spectrometer (VIRTIS) on board Venus Express. We show that the two emissions present very similar spatial structures. A…

2012 Icarus
VenusExpress 8
Latitudinal distribution of HDO abundance above Venus' clouds by ground-based 2.3 µm spectroscopy
DOI: 10.1016/j.icarus.2011.07.026 Bibcode: 2012Icar..217..610M

Matsui, H.; Iwagami, N.; Hosouchi, M. +2 more

The abundance of HDO above the clouds in the dayside atmosphere of Venus was measured by ground-based 2.3 µm spectroscopy over 4 days. This is the first HDO observation above the clouds in this wavelength region corresponding to a new height region. The latitudinal distributions found show no clearly defined structure. The disk-averaged mixi…

2012 Icarus
VenusExpress 7
Observation of DCl and upper limit to NH3 on Venus
DOI: 10.1016/j.icarus.2012.02.036 Bibcode: 2012Icar..219..244K

Krasnopolsky, Vladimir

To search for DCl in the Venus atmosphere, a spectrum near the D35Cl (1-0) R4 line at 2141.54 cm-1 was observed using the CSHELL spectrograph at NASA IRTF. Least square fitting to the spectrum by a synthetic spectrum results in a DCl mixing ratio of 17.8 ± 6.8 ppb. Comparing to the HCl abundance of 400 ± 30 ppb (Krasnopolsky …

2012 Icarus
VenusExpress 7
Zonal winds at high latitudes on Venus: An improved application of cyclostrophic balance to Venus Express observations
DOI: 10.1016/j.icarus.2011.07.010 Bibcode: 2012Icar..217..629M

Read, Peter L.; Mendonça, João M.; Wilson, Colin F. +1 more

Recent retrievals of zonal thermal winds obtained in a cyclostrophic regime on Venus are generally consistent with cloud tracking measurements at mid-latitudes, but become unphysical in polar regions where the values obtained above the clouds are often less than or close to zero. Using a global atmospheric model, we show that the main source of er…

2012 Icarus
VenusExpress 7
UV spectrum of Enceladus
DOI: 10.1016/j.icarus.2012.04.002 Bibcode: 2012Icar..220...29Z

Noll, Keith S.; Clarke, John T.; Hendrix, Amanda R. +1 more

We present a far ultraviolet (FUV) spectrum of Saturn’s moon Enceladus from the Cosmic Origins Spectrograph (COS) on the Hubble Space Telescope (HST). We have put upper limits on emission from C, N, and O lines in Enceladus’ atmosphere and column densities for the C lines assuming solar resonance scattering. We find these upper limits to be relati…

2012 Icarus
Cassini eHST 7
Improved luminosity model and albedo for Saturn
DOI: 10.1016/j.icarus.2011.11.035 Bibcode: 2012Icar..218...56M

Mallama, Anthony

The globe of Saturn is brighter than previously reported as indicated by its absolute opposition magnitudes in the UBVRI band passes which are -7.080, -7.842, -8.914, -9.587 and -9.606, respectively. The geometric albedo in V is 0.501 and it peaks in the R filter at 0.567. The brightest apparent magnitude of the system in the V-band is -0.61 and t…

2012 Icarus
eHST 7
Vertical cloud structure of the 2009 Jupiter impact based on HST/WFC3 observations
DOI: 10.1016/j.icarus.2012.10.012 Bibcode: 2012Icar..221.1061P

Sánchez-Lavega, A.; Pérez-Hoyos, S.; Wong, M. H. +7 more

The impact of a body of unknown origin with Jupiter in July 2009 produced an intense perturbation of the planet’s atmosphere at the visible cloud levels. The vertical cloud structure was deeply affected by the presence of a strongly absorbing dense aerosol layer that was expanded steadily by advection in the local winds. We observed this phenomeno…

2012 Icarus
eHST 7