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Altitude of Saturn's aurora and its implications for the characteristic energy of precipitated electrons
DOI: 10.1029/2008GL036554 Bibcode: 2009GeoRL..36.2202G

Bonfond, B.; Clarke, J. T.; Gérard, J. -C. +4 more

Images of Saturn's aurora at the limb have been collected with the Advanced Camera for Surveys on board the Hubble Space Telescope. They show that the peak of Saturn's nightside emission is generally located 900-1300 km above the 1-bar level. On the other hand, methane and H2 columns overlying the aurora have been determined from the an…

2009 Geophysical Research Letters
Cassini eHST 80
Ionospheric storms on Mars: Impact of the corotating interaction region
DOI: 10.1029/2008GL036559 Bibcode: 2009GeoRL..36.1105D

Barabash, S.; Lundin, R.; Woch, J. +5 more

Measurements made by the ASPERA-3 and MARSIS experiments on Mars Express have shown, for the first time, that space weather effects related to the impact of a dense and high pressure solar wind (corotating interaction region) on Mars cause strong perturbations in the martian induced magnetosphere and ionosphere. The magnetic barrier formed by pile…

2009 Geophysical Research Letters
MEx 65
A north-south difference in the rotation rate of auroral hiss at Saturn: Comparison to Saturn's kilometric radio emission
DOI: 10.1029/2009GL040774 Bibcode: 2009GeoRL..3621108G

Gurnett, D. A.; Persoon, A. M.; Hospodarsky, G. B. +3 more

Broadband whistler-mode emissions, commonly observed by the Cassini spacecraft at high latitudes in Saturn's magnetosphere at frequencies below about 100 Hz, have characteristics very similar to auroral hiss observed at high latitudes in Earth's magnetosphere. In contrast to terrestrial auroral hiss, which shows no obvious rotational modulation, S…

2009 Geophysical Research Letters
Cassini 64
Smoothness of Titan's Ontario Lacus: Constraints from Cassini RADAR specular reflection data
DOI: 10.1029/2009GL039588 Bibcode: 2009GeoRL..3616201W

Lorenz, R. D.; Wye, L. C.; Zebker, H. A.

Cassini RADAR altimetry data collected on the 49th flyby of Titan (2008 December 21) over Ontario Lacus in Titan's south polar region provides strong evidence for an extremely smooth surface, with less than 3 mm rms surface height variation over the 100m-wide Fresnel zone. Histograms of the raw radar echoes imply a mirror-like specular reflection …

2009 Geophysical Research Letters
Cassini 58
Cassini detection of Enceladus' cold water-group plume ionosphere
DOI: 10.1029/2009GL038923 Bibcode: 2009GeoRL..3613203T

Coates, A. J.; Thomsen, M. F.; Wilson, R. J. +6 more

This study reports direct detection by the Cassini plasma spectrometer of freshly-produced water-group ions (O+, OH+, H2O+, H3O+) and heavier water dimer ions (HxO2)+ very close to Enceladus where the plasma begins to emerge from the plume. The data …

2009 Geophysical Research Letters
Cassini 57
Amazonian-aged fluvial valley systems in a climatic microenvironment on Mars: Melting of ice deposits on the interior of Lyot Crater
DOI: 10.1029/2009GL037472 Bibcode: 2009GeoRL..36.8201D

Head, J. W.; Dickson, J. L.; Fassett, C. I.

Valley networks, regional drainage patterns suggesting liquid water stability at the surface, are confined to early in the history of Mars (the Noachian/Hesperian boundary and before), prior to a major climate transition to the hyperarid cold conditions of the Amazonian. Several later fluvial valley systems have been documented in specific Hesperi…

2009 Geophysical Research Letters
MEx 56
Detecting nanoparticles at radio frequencies: Jovian dust stream impacts on Cassini/RPWS
DOI: 10.1029/2008GL036752 Bibcode: 2009GeoRL..36.3103M

Gurnett, D. A.; Kaiser, M. L.; Meyer-Vernet, N. +1 more

We analyse wave observations by the Cassini/RPWS instrument performed during the Jovian fly-by, when the on-board dust analyser recorded dust streams which were interpreted as nanoparticles moving at about the solar wind speed. The observed wave pulses are produced by ionisation of dust grains impacting the spacecraft. Nanoparticles are detected b…

2009 Geophysical Research Letters
Cassini 56
Source regions of banded chorus
DOI: 10.1029/2009GL037629 Bibcode: 2009GeoRL..3611101B

Pickett, J. S.; Inan, U. S.; Bell, T. F. +1 more

ELF/VLF chorus emissions are very intense electromagnetic plasma waves that are naturally and spontaneously excited near the magnetic equatorial plane outside the plasmasphere during periods of magnetic disturbance. These emissions are believed to play an important role in the acceleration of 10 to 100 keV radiation belt electrons to MeV energies …

2009 Geophysical Research Letters
Cluster 56
Cassini RADAR images at Hotei Arcus and western Xanadu, Titan: Evidence for geologically recent cryovolcanic activity
DOI: 10.1029/2008GL036415 Bibcode: 2009GeoRL..36.4203W

Lorenz, R. D.; Janssen, M. A.; Lunine, J. I. +14 more

Images obtained by the Cassini Titan Radar Mapper (RADAR) reveal lobate, flowlike features in the Hotei Arcus region that embay and cover surrounding terrains and channels. We conclude that they are cryovolcanic lava flows younger than surrounding terrain, although we cannot reject the sedimentary alternative. Their appearance is grossly similar t…

2009 Geophysical Research Letters
Cassini 53
Periodicity in Saturn's magnetosphere: Plasma cam
DOI: 10.1029/2009GL039043 Bibcode: 2009GeoRL..3614203B

Young, D. T.; Burch, J. L.; DeJong, A. D. +1 more

Plasma ion data from the Cassini Plasma Spectrometer (CAPS) are examined for all orbits from October 25, 2004 through Dec. 26, 2007. To eliminate effects of incomplete angular coverage, data are only used from the CAPS anode that is closest to viewing into the corotational flow and within 20° of that flow. The data are plotted in the SKR-based SLS…

2009 Geophysical Research Letters
Cassini 52