Search Publications

The impact of turbulent vertical mixing in the Venus clouds on chemical tracers
DOI: 10.1016/j.icarus.2022.115148 Bibcode: 2022Icar..38615148L

Marcq, Emmanuel; Lefèvre, Franck; Lefèvre, Maxence

Venus' clouds host a convective layer between roughly 50 and 60 km that mixes heat, momentum, and chemical species. Observations and numerical modelling have helped to understand the complexity of this region. However, the impact on chemistry is still not known. Here, we use for the first time a three-dimensional convection-resolving model with pa…

2022 Icarus
VenusExpress 7
Discordance analysis on a high-resolution valley network map of Mars: Assessing the effects of scale on the conformity of valley orientation and surface slope direction
DOI: 10.1016/j.icarus.2022.115041 Bibcode: 2022Icar..38315041B

Bahia, Rickbir S.; Covey-Crump, Stephen; Jones, Merren A. +1 more

Fluvial valleys incised into planetary surfaces display morphologies, geometries and orientations that can be used to understand their controlling processes. Comparisons between valley orientations and topographic surface slope direction have been used to understand how Martian surfaces have evolved (Luo and Stepinski, 2012; Black et al., 2017); h…

2022 Icarus
MEx 6
Energy deposition in Saturn's equatorial upper atmosphere
DOI: 10.1016/j.icarus.2021.114724 Bibcode: 2022Icar..37214724C

Hu, X.; Galand, M.; Yelle, R. V. +6 more

We construct Saturn equatorial neutral temperature and density profiles of H, H2, He, and CH4, between 10-12 and 1 bar using measurements from Cassini's Ion Neutral Mass Spectrometer (INMS) taken during the spacecraft's final plunge into Saturn's atmosphere on 15 September 2017, combined with previous deeper atmosp…

2022 Icarus
SOHO 6
Investigating the most promising Yarkovsky candidates using Gaia DR2 astrometry
DOI: 10.1016/j.icarus.2022.115040 Bibcode: 2022Icar..38315040D

Oszkiewicz, Dagmara; Bartczak, Przemysław; Dziadura, Karolina

The Yarkovsky drift is a major factor driving the orbital evolution of asteroids. To date, the effect has been detected for a few hundred asteroids, mainly near-Earth objects. Before the start of the European Space Agency Gaia mission, the expectation was to recognize many other asteroids manifesting the Yarkovsky drift through the high precision …

2022 Icarus
Gaia 6
Machine learning as a tool to classify extra-terrestrial landslides: A dossier from Valles Marineris, Mars
DOI: 10.1016/j.icarus.2022.114886 Bibcode: 2022Icar..37614886R

Rajaneesh, A.; Vishnu, C. L.; Oommen, T. +2 more

Many researchers studied Martian landslides, and most of these studies are in the Valles Marineris (VM). Those studies are mainly morphologic analysis, estimates of landslide deposit volumes, thermal properties of the landslides, spectral analyses, and mapping and classifying landslides. But, this study created a robust landslide inventory of 682 …

2022 Icarus
MEx 6
Constraints on the uncertainty, timing, and magnitude of potential Mars oceans from topographic deformation models
DOI: 10.1016/j.icarus.2022.114934 Bibcode: 2022Icar..37814934S

Rivera-Hernández, Frances; Sholes, Steven F.

Proposed ocean paleoshorelines on Mars have faced criticism over their genetic interpretation and because they deviate significantly from an expected equipotential surface (by many kilometers). Multiple geophysical deformation models have been proposed to explain this large topographic range and deviation including true polar wander and direct Tha…

2022 Icarus
MEx 6
Investigating the origin of gypsum in Olympia Undae: Characterizing the mineralogy of the basal unit
DOI: 10.1016/j.icarus.2021.114720 Bibcode: 2022Icar..37214720D

Mustard, J. F.; Das, E.; Tarnas, J. D. +2 more

The Olympia Undae sand sea contains the largest known deposit of gypsum discovered on the surface of Mars. The origin of this gypsum, a hydrated sulfate mineral requiring liquid water for its formation, remains largely unconstrained. We examine the hypothesis that gypsum was derived from the early-Amazonian aged Basal Unit, which is suggested to c…

2022 Icarus
MEx 6
Atmospheric processes affecting methane on Mars
DOI: 10.1016/j.icarus.2022.114940 Bibcode: 2022Icar..38214940G

Rauer, H.; Arnold, G.; Herbst, K. +6 more

It is currently uncertain as to whether methane exists on Mars. Data from the Curiosity Rover suggests a background methane concentration of a few tenths parts per billion whereas data from the Trace Gas Orbiter suggest an upper limit of twenty parts per trillion. If methane exists on Mars then we do not understand fully the physical and chemical …

2022 Icarus
ExoMars-16 6
Convective storms in closed cyclones in Jupiter: (II) numerical modeling
DOI: 10.1016/j.icarus.2022.115169 Bibcode: 2022Icar..38615169I

Hueso, Ricardo; Sánchez-Lavega, Agustín; Legarreta, Jon +1 more

On May 31, 2020 a convective storm appeared in one small cyclone in the South Temperate Belt (STB) of Jupiter. The storm, nicknamed as Clyde's Spot, had an explosive start and quickly diminished in activity in a few days. However, it left a highly turbulent cyclone as a remnant that evolved to become a turbulent segment of the STB in a time-scale …

2022 Icarus
eHST 6
Numerical simulations of radar echoes rule out basal CO2 ice deposits at Ultimi Scopuli, Mars
DOI: 10.1016/j.icarus.2022.115163 Bibcode: 2022Icar..38615163O

Orosei, Roberto; Cartacci, Marco; Cicchetti, Andrea +10 more

The principal objective of the radar sounder MARSIS experiment is to look for ice and water in the Martian subsurface. One particular focus of investigations, since 2005, has been the search for basal liquid water in the south polar layered deposits (SPLD). Anomalously strong basal echoes detected from four distinct areas at the base of the deposi…

2022 Icarus
MEx 6