Search Publications

Age determination of linear surface features using the Buffered Crater Counting approach - Case studies of the Sirenum and Fortuna Fossae graben systems on Mars
DOI: 10.1016/j.icarus.2014.12.008 Bibcode: 2015Icar..250..384K

Platz, T.; Michael, G. G.; Walter, S. H. G. +1 more

Buffered Crater Counting (BCC) offers a possibility to determine ages of linear/curvilinear surface features that provide no or only very limited surface areas for the conventional crater counting approach. In this study we applied the BCC analysis to two tectonic fault systems, Fortuna Fossae and a subsection of Sirenum Fossae. We compared BCC re…

2015 Icarus
MEx 59
Record-breaking storm activity on Uranus in 2014
DOI: 10.1016/j.icarus.2014.12.037 Bibcode: 2015Icar..252..121D

de Pater, Imke; Sromovsky, L. A.; Fry, P. M. +3 more

In spite of an expected decline in convective activity following the 2007 equinox of Uranus, eight sizable storms were detected on the planet with the near-infrared camera NIRC2, coupled to the adaptive optics system, on the 10-m W.M. Keck telescope on UT 5 and 6 August 2014. All storms were on Uranus' northern hemisphere, including the brightest …

2015 Icarus
eHST 55
Detection of Callisto's oxygen atmosphere with the Hubble Space Telescope
DOI: 10.1016/j.icarus.2015.03.021 Bibcode: 2015Icar..254..178C

France, Kevin; Feldman, Paul D.; Strobel, Darrell F. +3 more

We report the result of a search for evidence of an O2-dominated atmosphere on Callisto, using the high far-ultraviolet sensitivity of the Hubble Space Telescope Cosmic Origins Spectrograph (COS). Observations of Callisto's leading/Jupiter-facing hemisphere show, for the first time, variable-strength atomic oxygen (O I) emissions with b…

2015 Icarus
eHST 54
Mixtures of clays and sulfates within deposits in western Melas Chasma, Mars
DOI: 10.1016/j.icarus.2014.04.009 Bibcode: 2015Icar..251..291W

Wray, James J.; Weitz, Catherine M.; Noe Dobrea, Eldar

We have utilized several data sets from multiple spacecraft that have been acquired over a continuous observation campaign across the southwestern Melas Chasma region of Mars. The blocky deposit observed on the chasma floor and on portions of the southern wallrock consists of mixtures of light- and medium-toned materials that exhibit displacement …

2015 Icarus
MEx 53
Thermal evolution of Venus with argon degassing
DOI: 10.1016/j.icarus.2015.07.009 Bibcode: 2015Icar..260..128O

O'Rourke, Joseph G.; Korenaga, Jun

Decades-old measurements of atmospheric and elemental surface composition constrain the history of Venus. In this study, we search for a model featuring continuous evolution in the stagnant-lid regime that predicts the present-day atmospheric mass of radiogenic argon and satisfies the other available constraints. For comparison, we also consider t…

2015 Icarus
VenusExpress 52
Dust devil height and spacing with relation to the martian planetary boundary layer thickness
DOI: 10.1016/j.icarus.2015.07.028 Bibcode: 2015Icar..260..246F

Fenton, Lori K.; Lorenz, Ralph

In most remote and unmonitored places, little is known about the characteristics of daytime turbulent activity. Few processes render the optically transparent atmospheres of Earth and Mars visible; put more plainly, without clever instruments it is difficult to "see the unseen". To address this, we present a pilot study of images of martian dust d…

2015 Icarus
MEx 51
Lithospheric structure of Venus from gravity and topography
DOI: 10.1016/j.icarus.2015.07.020 Bibcode: 2015Icar..260..215J

Ruiz, Javier; Jiménez-Díaz, Alberto; Kirby, Jon F. +3 more

There are many fundamental and unanswered questions on the structure and evolution of the venusian lithosphere, which are key issues for understanding Venus in the context of the origin and evolution of the terrestrial planets. Here we investigate the lithospheric structure of Venus by calculating its crustal and effective elastic thicknesses (T

2015 Icarus
VenusExpress 49
A radar survey of M- and X-class asteroids. III. Insights into their composition, hydration state, & structure
DOI: 10.1016/j.icarus.2014.09.016 Bibcode: 2015Icar..245...38S

Nolan, Michael C.; Springmann, Alessondra; Howell, Ellen S. +13 more

Using the S-band radar at Arecibo Observatory, we observed thirteen X/M-class asteroids; nine were previously undetected and four were re-observed, bringing the total number of Tholen X/M-class asteroids observed with radar to 29. Of these 29M-class asteroids, 13 are also W-class, defined as M-class objects that also display a 3-µm absorptio…

2015 Icarus
AKARI 47
Orbital detection and implications of akaganéite on Mars
DOI: 10.1016/j.icarus.2015.01.020 Bibcode: 2015Icar..253..296C

Le Deit, Laetitia; Carter, John; Loizeau, Damien +2 more

The martian surface bears the mineralogical record of ancient sub-surface and surface aqueous alteration environments. While most of the chemical alteration produced phyllosilicates, hydrated sulfates and chlorides, other less common compounds provide key constraints on localized geochemical settings, and help refine the geological evolution of th…

2015 Icarus
MEx 45
Sulfur in the early martian atmosphere revisited: Experiments with a 3-D Global Climate Model
DOI: 10.1016/j.icarus.2015.08.011 Bibcode: 2015Icar..261..133K

Forget, François; Kerber, Laura; Wordsworth, Robin

Volcanic SO2 in the martian atmosphere has been invoked as a way to create a sustained or transient greenhouse during early martian history. Many modeling studies have been performed to test the feasibility of this hypothesis, resulting in a range of conclusions, from highly feasible to highly improbable. In this study we perform a wide…

2015 Icarus
MEx 45