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Connections between spectra and structure in Saturn’s main rings based on Cassini VIMS data
DOI: 10.1016/j.icarus.2012.10.014 Bibcode: 2013Icar..223..105H

Clark, R. N.; Nicholson, P. D.; Hedman, M. M. +4 more

Saturn’s main rings exhibit variations in both their opacity and their spectral properties on a broad range of spatial scales, and the correlations between these parameters can provide insights into the processes that shape the composition and dynamics of the rings. The Visual and Infrared Mapping Spectrometer (VIMS) instrument onboard the Cassini…

2013 Icarus
Cassini 50
Saturn’s Great Storm of 2010-2011: Evidence for ammonia and water ices from analysis of VIMS spectra
DOI: 10.1016/j.icarus.2013.05.043 Bibcode: 2013Icar..226..402S

Baines, K. H.; Sromovsky, L. A.; Fry, P. M.

Our analysis of Cassini/VIMS near-infrared spectra of Saturn’s Great Storm of 2010-2011 reveals a multi-component aerosol composition comprised primarily of ammonia ice, with a significant component of water ice. The most likely third component is ammonium hydrosulfide or some weakly absorbing material similar to what dominates visible clouds outs…

2013 Icarus
Cassini 50
Near-infrared spectral monitoring of Pluto's ices: Spatial distribution and secular evolution
DOI: 10.1016/j.icarus.2013.01.019 Bibcode: 2013Icar..223..710G

Olkin, C. B.; Buie, M. W.; Young, E. F. +2 more

We report results from monitoring Pluto's 0.8 to 2.4 µm reflectance spectrum with IRTF/SpeX on 65 nights over the dozen years from 2001 to 2012. The spectra show vibrational absorption features of simple molecules CH4, CO, and N2 condensed as ices on Pluto's surface. These absorptions are modulated by the planet's 6.39 …

2013 Icarus
eHST 49
Observations of D/H ratios in H2O, HCl, and HF on Venus and new DCl and DF line strengths
DOI: 10.1016/j.icarus.2013.02.010 Bibcode: 2013Icar..224...57K

Li, G.; Belyaev, D. A.; Krasnopolsky, V. A. +2 more

Intensities of the spectral lines in the fundamental bands of D35Cl and DF were calculated using the semi-empirical dipole moment functions derived from the most accurate and precise measurements of intensities of the ro-vibrational lines of H35Cl and HF. Values obtained in this way for the deuterated species are superior to …

2013 Icarus
VenusExpress 49
Multiple working hypotheses for the formation of compositional stratigraphy on Mars: Insights from the Mawrth Vallis region
DOI: 10.1016/j.icarus.2013.05.024 Bibcode: 2013Icar..226..816M

Baldridge, A. M.; Michalski, Joseph R.; Cuadros, J. +1 more

A unique aspect of martian geology is the presence of similar compositional stratigraphy observed in many locations throughout the surface. Where the Al-rich and Fe/Mg-rich clay minerals occur together, aluminous clays typically overly layered ferromagnesian clays, possibly indicating that precipitation-driven leaching occurred in a warmer, wetter…

2013 Icarus
MEx 47
Evidence for two modes of water release in Comet 103P/Hartley 2: Distributions of column density, rotational temperature, and ortho-para ratio
DOI: 10.1016/j.icarus.2012.07.034 Bibcode: 2013Icar..222..740B

Villanueva, Geronimo L.; Mumma, Michael J.; Meech, Karen J. +5 more

This paper presents long-slit spectra of H2O emission from the inner coma of Comet 103P/Hartley 2, acquired with NIRSPEC/Keck 2 during the comet's close approach to Earth in 2010. On UT 19.6 October 2010 the slit was oriented nearly orthogonal to the projected (in the plane of the sky) Sun-comet line, and the H2O rotational t…

2013 Icarus
ISO 47
Impact basin relaxation on Rhea and Iapetus and relation to past heat flow
DOI: 10.1016/j.icarus.2013.01.013 Bibcode: 2013Icar..223..699W

Schenk, Paul M.; White, Oliver L.; Dombard, Andrew J.

Evidence for relaxation of impact crater topography has been observed on many icy satellites, including those of Saturn, and the magnitude of relaxation can be related to past heat flow (e.g. Moore, J.M., Schenk, P.M., Bruesch, L.S., Asphaug, E., McKinnon, W.B. [2004]. Icarus 171, 421-443; Dombard, A.J., McKinnon, W.B. [2006]. J. Geophys. Res. 111…

2013 Icarus
Cassini 47
Crater topography on Titan: Implications for landscape evolution
DOI: 10.1016/j.icarus.2012.11.030 Bibcode: 2013Icar..223...82N

Lorenz, R. D.; Kirk, R. L.; Cassini Radar Team +7 more

We present a comprehensive review of available crater topography measurements for Saturn’s moon Titan. In general, the depths of Titan’s craters are within the range of depths observed for similarly sized fresh craters on Ganymede, but several hundreds of meters shallower than Ganymede’s average depth vs. diameter trend. Depth-to-diameter ratios a…

2013 Icarus
Cassini 46
Processes forming and sustaining Saturn's proton radiation belts
DOI: 10.1016/j.icarus.2012.10.033 Bibcode: 2013Icar..222..323K

Krupp, N.; Roussos, E.; Paranicas, C. +2 more

Saturn's proton radiation belts extend over the orbits of several moons that split this region of intense radiation into several distinct belts. Understanding their distribution requires to understand how their particles are created and evolve. High-energy protons are thought to be dominantly produced by cosmic ray albedo neutron decay (CRAND). Th…

2013 Icarus
Cassini 43
Wind driven capillary-gravity waves on Titan's lakes: Hard to detect or non-existent?
DOI: 10.1016/j.icarus.2013.04.004 Bibcode: 2013Icar..225..403H

Lorenz, R. D.; Lunine, J. I.; Hayes, A. G. +13 more

Saturn's moon Titan has lakes and seas of liquid hydrocarbon and a dense atmosphere, an environment conducive to generating wind waves. Cassini observations thus far, however, show no indication of waves. We apply models for wind wave generation and detection to the Titan environment. Results suggest wind speed thresholds at a reference altitude o…

2013 Icarus
Cassini 42