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The dust trail of Comet 67P/Churyumov-Gerasimenko between 2004 and 2006
DOI: 10.1016/j.icarus.2010.01.003 Bibcode: 2010Icar..207..992A

Reach, William T.; Agarwal, Jessica; Grün, Eberhard +3 more

We report on observations of the dust trail of Comet 67P/Churyumov-Gerasimenko (CG) in visible light with the Wide Field Imager at the ESO/MPG 2.2 m telescope at 4.7 AU before aphelion, and at 24µm with the MIPS instrument on board the Spitzer Space Telescope at 5.7 AU both before and after aphelion. The comet did not appear to be active dur…

2010 Icarus
Rosetta 61
Large density fluctuations in the martian ionosphere as observed by the Mars Express radar sounder
DOI: 10.1016/j.icarus.2009.02.019 Bibcode: 2010Icar..206...83G

Gurnett, D. A.; Barabash, S.; Winningham, J. D. +5 more

The MARSIS (Mars Advanced Radar for Subsurface and Ionosphere Sounding) instrument on the Mars Express spacecraft provides both local and remote measurements of electron densities and measurements of magnetic fields in the martian ionosphere. The density measurements show a persistent level of large fluctuations, sometimes as much as a factor of t…

2010 Icarus
MEx 60
Impact cratering records of the mid-sized, icy saturnian satellites
DOI: 10.1016/j.icarus.2009.12.007 Bibcode: 2010Icar..206..485K

Schenk, Paul; Kirchoff, Michelle R.

Resolution of Voyager 1 and 2 images of the mid-sized, icy saturnian satellites was generally not much better than 1 km per line pair, except for a few, isolated higher resolution images. Therefore, analyses of impact crater distributions were generally limited to diameters ( D) of tens of kilometers. Even with the limitation, however, these analy…

2010 Icarus
Cassini 60
Saturn’s icy satellites investigated by Cassini-VIMS. II. Results at the end of nominal mission
DOI: 10.1016/j.icarus.2009.11.006 Bibcode: 2010Icar..206..507F

Brown, R. H.; Buratti, B. J.; Clark, R. N. +12 more

We report the detailed analysis of the spectrophotometric properties of Saturn's icy satellites as derived by full-disk observations obtained by visual and infrared mapping spectrometer (VIMS) experiment aboard Cassini. In this paper, we have extended the coverage until the end of the Cassini's nominal mission (June 1st 2008), while a previous pap…

2010 Icarus
Cassini 60
Titan haze distribution and optical properties retrieved from recent observations
DOI: 10.1016/j.icarus.2010.03.016 Bibcode: 2010Icar..208..850R

Le Mouélic, S.; Rodriguez, S.; Sotin, C. +4 more

The VIMS instrument onboard Cassini observed the north polar region of Titan at 113° phase angle, 28 December 2006. On this spectral image, a vast polar cloud can be seen northward to 62°N, and elsewhere, the haze appears as the dominant source of scattering. Because the surface does not appear in the wavelength range between 0.3 and 4.9µm, …

2010 Icarus
Cassini 58
Aeolian processes and dune morphology in Gale Crater
DOI: 10.1016/j.icarus.2010.06.006 Bibcode: 2010Icar..210..102H

Hobbs, Steven W.; Paull, David J.; Bourke, Mary C.

Datasets at resolutions many times greater than previously available were used to study aeolian features within Gale Crater. High resolution thermal inertia data allowed for detailed particle size estimation, with the data sufficient to resolve dunefields. A wide range of grain sizes have now been identified in the Gale Crater dunefields, ranging …

2010 Icarus
MEx 57
Spatially-resolved high-resolution spectroscopy of Venus 2. Variations of HDO, OCS, and SO 2 at the cloud tops
DOI: 10.1016/j.icarus.2010.05.008 Bibcode: 2010Icar..209..314K

Krasnopolsky, Vladimir A.

While CO, HCl, and HF, that were considered in the first part of this work, have distinct absorption lines in high-resolution spectra and were detected four decades ago, the lines of HDO, OCS, and SO 2 are either very weak or blended by the telluric lines and have not been observed previously by ground-based infrared spectroscopy at the…

2010 Icarus
VenusExpress 57
Subsurface heat transfer on Enceladus: Conditions under which melting occurs
DOI: 10.1016/j.icarus.2009.09.015 Bibcode: 2010Icar..206..594I

Ingersoll, Andrew P.; Pankine, Alexey A.

Given the heat that is reaching the surface from the interior of Enceladus, we ask whether liquid water is likely and at what depth it might occur. The heat may be carried by thermal conduction through the solid ice, by the vapor as it diffuses through a porous matrix, or by the vapor flowing upward through open cracks. The vapor carries latent he…

2010 Icarus
Cassini 56
Thermal structure and composition of Jupiter’s Great Red Spot from high-resolution thermal imaging
DOI: 10.1016/j.icarus.2010.01.005 Bibcode: 2010Icar..208..306F

Fletcher, Leigh N.; Hayward, T. L.; Irwin, P. G. J. +11 more

Thermal-IR imaging from space-borne and ground-based observatories was used to investigate the temperature, composition and aerosol structure of Jupiter's Great Red Spot (GRS) and its temporal variability between 1995 and 2008. An elliptical warm core, extending over 8° of longitude and 3° of latitude, was observed within the cold anticyclonic vor…

2010 Icarus
eHST 56
Persistent rings in and around Jupiter’s anticyclones - Observations and theory
DOI: 10.1016/j.icarus.2010.07.027 Bibcode: 2010Icar..210..742D

de Pater, Imke; Wong, Michael H.; Luszcz-Cook, Statia +5 more

We present observations and theoretical calculations to derive the vertical structure of and secondary circulation in jovian vortices, a necessary piece of information to ultimately explain the red color in the annular ring inside Jupiter's Oval BA. The observations were taken with the near-infrared detector NIRC2 coupled to the adaptive optics sy…

2010 Icarus
eHST 55