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A Mars orbital catalog of aqueous alteration signatures (MOCAAS)
DOI: 10.1016/j.icarus.2022.115164 Bibcode: 2023Icar..38915164C

Bibring, Jean-Pierre; Langevin, Yves; Gondet, Brigitte +3 more

We describe the completion of the MOCAAS project providing a global repository of secondary minerals formed through interaction with water on Mars. This work is based on the analysis of orbital imaging spectroscopy data from the OMEGA/Mars Express and CRISM/MRO near-infrared instruments. A database and a set of high-resolution global maps (200 m/p…

2023 Icarus
MEx 24
Solar cycle variation of ion escape from Mars
DOI: 10.1016/j.icarus.2021.114610 Bibcode: 2023Icar..39314610N

Barabash, Stas; Nilsson, Hans; Zhang, Qi +6 more

Using Mars Express data from 2007 until 2020 we show how ion outflow from Mars varied over more than a solar cycle, from one solar minimum to another. The data was divided into intervals with a length of one Martian year, starting from 30 April 2007 and ending 13 July 2020. The net escape rate was about 5 × 1024s-1 in the fir…

2023 Icarus
MEx 12
The effects of atmospheric dust and solar radiation on the dayside ionosphere of Mars derived from 17 years of Mars Express radio science observations
DOI: 10.1016/j.icarus.2023.115565 Bibcode: 2023Icar..40015565P

Pätzold, M.; González-Galindo, F.; Witasse, O. +5 more

This work combines 17 years of Mars Express radio science (MaRS) observations with proxies for insolation and local/global atmospheric dust to investigate the combined and individual effects on the dayside ionosphere of Mars from the top down to the ionospheric base.

The increase in insolation from orbital apocenter to pericenter in combinati…

2023 Icarus
MEx 5
Morphology and paleohydrology of intracrater alluvial fans north of Hellas Basin, Mars
DOI: 10.1016/j.icarus.2022.115122 Bibcode: 2023Icar..39415122A

Williams, Rebecca M. E.; Anderson, Ryan B.; Gullikson, Amber L. +1 more

Alluvial fans and sinuous ridges are both important records of the history of fluvial activity on Mars, and they often occur together. We present observations of alluvial fans, many of which exhibit inverted relief, in five craters in the region north of Hellas basin. The observed fans ranged in size from ~10 to 820 km2. We identified t…

2023 Icarus
MEx 5
The brightness of the CO Cameron bands in the martian discrete aurora: A study based on revised cross sections
DOI: 10.1016/j.icarus.2023.115602 Bibcode: 2023Icar..40215602G

Daerden, F.; Neary, L.; Gérard, J. -C. +2 more

We analyze the consequences of the new laboratory measurements of the emissions cross sections of the Cameron bands excited by electron impact on CO2 and CO in the Mars aurora. We use Monte Carlo simulations to investigate the importance of these changes and their dependence on the initial electron energy. The Mars Climate Database (MCD…

2023 Icarus
MEx 4
Differential apparent thermal inertia of sloping terrain on Mars: Implications for the magmatic intrusions at Olympus Mons
DOI: 10.1016/j.icarus.2022.115283 Bibcode: 2023Icar..38915283C

Ciazela, M.; Ciazela, J.; Pieterek, B.

Mars, which exhibits exceptionally high surface temperature gradients due to the lack of vegetation and thin atmosphere, is especially suitable for the DATI approach. Taking advantage of this Mars property, we propose a new DATI-based method for thermal inertia calculation on Mars based on albedo and short-time-intervals of temperature difference.…

2023 Icarus
MEx 3
An updated global survey of alluvial fans on Mars: Distinguishing alluvial fans from other fan-shaped features through morphologic characterization
DOI: 10.1016/j.icarus.2022.115238 Bibcode: 2023Icar..38915238M

Moersch, Jeffrey E.; Mondro, Claire A.; Fedo, Christopher M.

Alluvial fans formed on Mars during the late Hesperian to early Amazonian in a climatic transition from a time of regular surface water activity to the current dry and cold climate. The depositional environments recorded by alluvial fans represent the final era of potential habitability on the Martian surface. Alluvial fan deposits can often look …

2023 Icarus
MEx 3
Assessing slope uncertainties of martian Digital Elevation Models from numerical propagation of errors on synthetic geological surfaces
DOI: 10.1016/j.icarus.2022.115341 Bibcode: 2023Icar..39115341M

Quantin-Nataf, C.; Leyrat, C.; Millot, C. +2 more

Digital Elevation Models (DEM) are widely used in planetary sciences, including for the specific case of Mars. DEMs allow us to extract topography parameters necessary in geomorphological studies. However, DEMs are not free from vertical errors, which yields uncertainties in calculations of parameters such as local slopes. In addition, slope maps …

2023 Icarus
ExoMars-16 MEx 3
OMEGA/Mars Express: A new martian atmospheric dust hunter
DOI: 10.1016/j.icarus.2022.115366 Bibcode: 2023Icar..39215366L

Vincendon, Mathieu; Leseigneur, Yann

While dust is a key parameter of Mars climate, its behaviour from one year to the next can appear erratic. This variability is notably related to Global Dust Storms (GDS) which occur only certain years with different onset, duration and intensity. The interannual variabilities of the dust cycle may notably explain some characteristics of Recurring…

2023 Icarus
MEx 3
Ionosphere of Mars during the consecutive solar minima 23/24 and 24/25 as seen by MARSIS-Mars Express
DOI: 10.1016/j.icarus.2021.114616 Bibcode: 2023Icar..39314616S

Witasse, Olivier; Sánchez-Cano, Beatriz; Kofman, Wlodek +4 more

The Mars' ionospheric behavior during two consecutive solar minima (23/24 and 24/25) is investigated with the same dataset. In particular, we use the Mars Advanced Radar for Subsurface and Ionospheric Sounding (MARSIS) on board Mars Express to investigate the total electron content behavior of the whole atmosphere in relation to the solar irradian…

2023 Icarus
MEx 3