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Clay sediments derived from fluvial activity in and around Ladon basin, Mars
DOI: 10.1016/j.icarus.2022.115090 Bibcode: 2022Icar..38415090W

Weitz, Catherine M.; Wilson, Sharon A.; Grant, John A. +5 more

The morphology and mineralogy of light-toned layered sedimentary deposits were investigated using multiple orbital datasets across the Ladon basin region, including within northern Ladon Valles, southern Ladon basin, and the southwestern highlands of Ladon basin. Light-toned layered deposits are particularly widespread in Ladon Valles and Ladon ba…

2022 Icarus
MEx 4
High-resolution DTM-based estimation of geomorphometric parameters of selected putative martian scoria cones
DOI: 10.1016/j.icarus.2022.114923 Bibcode: 2022Icar..37714923V

Székely, Balázs; Vörös, Fanni

Some previous studies have identified a number of features on Mars that are thought to be scoria cones. Since (terrestrial) scoria cones have special significance that they are monogenetic volcanoes, i.e. the volcanic edifice is created by a single eruptive event. The process usually produces fairly symmetrical cones, making them a target for morp…

2022 Icarus
MEx 4
Modeling the complete set of Cassini's UVIS occultation observations of Enceladus' plume
DOI: 10.1016/j.icarus.2022.114918 Bibcode: 2022Icar..38314918P

Esposito, Larry W.; Portyankina, Ganna; Aye, Klaus-Michael +2 more

The Cassini Ultraviolet Imaging Spectrograph (UVIS) observed a plume of water vapor spewing out from the south polar regions of Enceladus via occultations 7 times during the Cassini mission. Five of them yielded spatially resolved data that allowed fits to a set of individually modeled jets. We created a direct simulation Monte Carlo (DSMC) model …

2022 Icarus
Cassini 3
Geology of the Crüger-Sirsalis Basin: Evidence for prolonged volcanism in the southwestern near side of the Moon
DOI: 10.1016/j.icarus.2021.114875 Bibcode: 2022Icar..37614875S

Bhatt, Megha; Bhardwaj, Anil; Srivastava, Neeraj +1 more

The Pre-Nectarian Crüger-Sirsalis Basin (centered at 16.0°S, 293.0°E; ~ 475 km in diameter) is a primarily degraded and obscured impact basin on the Moon. This study presents the first geological description of the Crüger-Sirsalis Basin using remote sensing datasets from Lunar Reconnaissance Orbiter (LRO), Chandrayaan-1, and Kaguya missions. An in…

2022 Icarus
Chandrayaan-1 2
The stability of a liquid-water body below the south polar cap of Mars
DOI: 10.1016/j.icarus.2022.115073 Bibcode: 2022Icar..38315073E

Ruiz, Javier; Bramson, Ali M.; Egea-González, Isabel +4 more

Radar data from the Mars Express spacecraft show bright subsurface reflections in the Planum Australe area that could be due to liquid water located at a depth of 1.5 km (Orosei et al., 2018). If this interpretation of the data is correct, the presence of such water would have important implications for the present-day thermal state of the region.…

2022 Icarus
MEx 2
Invited review: Infrared spectroscopy of planetary atmospheres: Searching for insights into their past and present histories
DOI: 10.1016/j.icarus.2022.114885 Bibcode: 2022Icar..37614885E

Encrenaz, Thérèse

This article reflects my personal experience and illustrates some developments in the field of planetary spectroscopy, achieved within the Planetology Group of Paris Observatory over the past fifty years. Over these decades, planetary spectroscopy has led to the identification of minor atmospheric species with mixing ratios as low as a few parts p…

2022 Icarus
ISO 2
Astrometric observations and analysis of Triton during 2013-2019
DOI: 10.1016/j.icarus.2021.114728 Bibcode: 2022Icar..37214728Y

Zhang, H. Y.; Yan, D.; Qiao, R. C. +2 more

Triton is the largest irregular satellite of Neptune. A total of 1135 new observed positions of Triton in the period 2013-2019 were collected by the 1.0 m telescopes at Yunnan Astronomical Observatory of CAS during 13 nights. These positions of Triton were obtained based on Gaia DR2 catalogue. We compared our observations to the theoretical positi…

2022 Icarus
Gaia 2
Molecular hydrogen in the upper atmospheres of Saturn and Titan
DOI: 10.1016/j.icarus.2021.114876 Bibcode: 2022Icar..37614876S

Strobel, Darrell F.

Molecular hydrogen is the third most abundant species in Titan's atmosphere with a tropospheric/lower stratospheric mole fraction of 0.001 derived from Voyager and Cassini measurements and the major species in Saturn's atmosphere. The motivation for this paper is to explore the hypothesis that the corrected H2 density measurements repor…

2022 Icarus
Cassini 2
Early Noachian terrains: Vestiges of the early evolution of Mars
DOI: 10.1016/j.icarus.2022.115170 Bibcode: 2022Icar..38715170A

Dohm, James M.; Buczkowski, Debra; Anderson, Robert C. +1 more

NASA's main scientific reason for exploring Mars is to determine the early evolution and the possibility of life on the red planet. Scientists have adopted an approach for identifying habitable environments on Mars that could be conducive to the early development and preservation of life (e.g., robotically exploring hydrothermal and lake deposits …

2022 Icarus
MEx 2
Venus mountain waves in the upper atmosphere simulated by a time-invariant linear full-wave spectral model
DOI: 10.1016/j.icarus.2022.114922 Bibcode: 2022Icar..37714922H

Schubert, Gerald; Navarro, Thomas; Walterscheid, Richard L. +1 more

A 2-D spectral full-wave model is described that simulates the generation and propagation of mountain waves over idealized topography in Venus' atmosphere. Modeled temperature perturbations are compared with the Akatsuki observations. Lower atmosphere eddy diffusivity and stability play a major role in the upward propagation of gravity waves from …

2022 Icarus
VenusExpress 2