Search Publications

SOHO/SWAN observations of comets with small perihelia: C/2002 V1 (NEAT), C/2002 X5 (Kudo-Fujikawa), 2006 P1 (McNaught) and 96P/Machholz 1
DOI: 10.1016/j.icarus.2011.09.019 Bibcode: 2011Icar..216..449C

Bertaux, J. -L.; Combi, M. R.; Quémerais, E. +4 more

SWAN, the all-sky hydrogen Lyman-alpha camera on the SOHO spacecraft, designed primarily to image the interplanetary neutral hydrogen around the Sun, also observes comets continuously over large portions of their apparitions to the north and south of the ecliptic and at small solar elongation angles. Because of SOHO’s location at the L1 Lagrange p…

2011 Icarus
SOHO 14
Vertical profile of H 2SO 4 vapor at 70-110 km on Venus and some related problems
DOI: 10.1016/j.icarus.2011.06.036 Bibcode: 2011Icar..215..197K

Krasnopolsky, Vladimir A.

The vertical profile of H 2SO 4 vapor is calculated using current atmospheric and thermodynamic data. The atmospheric data include the H 2O profiles observed at 70-112 km by the SOIR solar occultations, the SPICAV-UV profiles of the haze extinction at 220 nm, the VeRa temperature profiles, and a typical profile of …

2011 Icarus
VenusExpress 14
Preservation of Late Amazonian Mars ice and water-related deposits in a unique crater environment in Noachis Terra: Age relationships between lobate debris tongues and gullies
DOI: 10.1016/j.icarus.2010.08.004 Bibcode: 2011Icar..211..347M

Head, James W.; Marchant, David R.; Morgan, Gareth A.

The Amazonian period of Mars has been described as static, cold, and dry. Recent analysis of high-resolution imagery of equatorial and mid-latitude regions has revealed an array of young landforms produced in association with ice and liquid water; because near-surface ice in these regions is currently unstable, these ice-and-water-related landform…

2011 Icarus
MEx 14
On Titan's Xanadu region
DOI: 10.1016/j.icarus.2011.03.018 Bibcode: 2011Icar..214..556B

Barnes, Jason W.; Brown, Robert H.; Melosh, H. Jay

A large, circular marking ∼1800 km across is seen in near-infrared images of Titan. The feature is centered at 10°S, 120°W on Titan, encompasses much of Titan's western Xanadu region, and has an off-center, quasi-circular, inner margin about 700 km across, with lobate outer margins extending 200-500 km from the inner margin. On the feature's south…

2011 Icarus
Cassini 13
Comparison of PFS and TES observations of temperature and water vapor in the martian atmosphere
DOI: 10.1016/j.icarus.2011.07.032 Bibcode: 2011Icar..215..628W

Smith, Michael D.; Formisano, Vittorio; Wolkenberg, Paulina +1 more

The interval from L s = 330° in Mars Year (MY) 26 until L s = 84° in MY 27 has been used to compare and validate measurements from the Mars Global Surveyor Thermal Emission Spectrometer (TES) and the Mars Express Planetary Fourier Spectrometer (PFS). We studied differences between atmospheric temperatures observed by the two …

2011 Icarus
MEx 13
Evidence for paleolakes in Erythraea Fossa, Mars: Implications for an ancient hydrological cycle
DOI: 10.1016/j.icarus.2011.03.004 Bibcode: 2011Icar..213..104B

Head, James W.; Fassett, Caleb I.; Buhler, Peter B. +1 more

There is now widespread agreement that the surface of Mars underwent some degree of fluvial modification, but there is not yet full understanding of its surface hydrological cycle and the nature of standing bodies of water, rivers, and precipitation that affected its surface. In this paper we explore Erythraea Fossa (31.5 W, 27.3 S), a graben adja…

2011 Icarus
MEx 13
Long-term evolution of the aerosol debris cloud produced by the 2009 impact on Jupiter
DOI: 10.1016/j.icarus.2011.03.015 Bibcode: 2011Icar..214..462S

Hueso, R.; Sánchez-Lavega, A.; Fletcher, L. N. +43 more

We present a study of the long-term evolution of the cloud of aerosols produced in the atmosphere of Jupiter by the impact of an object on 19 July 2009 (Sánchez-Lavega, A. et al. [2010]. Astrophys. J. 715, L155-L159). The work is based on images obtained during 5 months from the impact to 31 December 2009 taken in visible continuum wavelengths and…

2011 Icarus
eHST 12
Search for and limits on plume activity on Mimas, Tethys, and Dione with the Cassini Visual Infrared Mapping Spectrometer (VIMS)
DOI: 10.1016/j.icarus.2011.04.030 Bibcode: 2011Icar..214..534B

Brown, R. H.; Baines, K. H.; Buratti, B. J. +4 more

Cassini Visual Infrared Mapping Spectrometer (VIMS) observations of Mimas, Tethys, and Dione obtained during the nominal and extended missions at large solar phase angles were analyzed to search for plume activity. No forward scattered peaks in the solar phase curves of these satellites were detected. The upper limit on water vapor production for …

2011 Icarus
Cassini 12
Lithological mapping of central part of Mare Moscoviense using Chandrayaan-1 Hyperspectral Imager (HySI) data
DOI: 10.1016/j.icarus.2011.02.006 Bibcode: 2011Icar..212..470B

Bhattacharya, Satadru; Chauhan, Prakash; Ajai +2 more

We conducted spectral analysis of central region of the Mare Moscoviense area on the far side of the Moon using the Hyperspectral Imager (HySI) data from the Chandrayaan-1 mission in an effort to identify and map the major lithological units present in the area. Various spectral band parameters, namely, band curvature, band tilt and band strength …

2011 Icarus
Chandrayaan-1 12
Ultraviolet spectroscopy of Asteroid (4) Vesta
DOI: 10.1016/j.icarus.2011.10.003 Bibcode: 2011Icar..216..640L

A'Hearn, Michael F.; Feaga, Lori M.; Russell, Christopher T. +6 more

We report a comprehensive review of the UV-visible spectrum and rotational lightcurve of Vesta combining new observations by Hubble Space Telescope and Swift Gamma-ray Burst Observatory with archival International Ultraviolet Explorer observations. The geometric albedos of Vesta from 220 nm to 953 nm are derived by carefully comparing these observ…

2011 Icarus
IUE eHST 10