Search Publications

The global distribution and morphologic characteristics of fan-shaped sedimentary landforms on Mars
DOI: 10.1016/j.icarus.2022.115137 Bibcode: 2022Icar..38515137M

Wilson, Sharon A.; Howard, Alan D.; Morgan, Alexander M.

Fan-shaped sedimentary landforms on Mars are important geomorphic markers of past water flow and characterizing the distribution and morphology of these features can yield insights into the planet's climatic evolution. We present a new database of 1501 martian fan-shaped sedimentary landforms that builds upon previous surveys and uses Context Came…

2022 Icarus
MEx 16
Troposphere-to-mesosphere microphysics of carbon dioxide ice clouds in a Mars Global Climate Model
DOI: 10.1016/j.icarus.2022.115098 Bibcode: 2022Icar..38515098M

Forget, F.; Montmessin, F.; González-Galindo, F. +10 more

We have implemented full CO2 ice cloud microphysics into the LMD Mars Global Climate Model (MGCM) and we have conducted the first global simulations. The microphysical model implementation follows the modal scheme used for water ice cloud microphysics in the MGCM, but includes specific aspects that need to be accounted for when dealing …

2022 Icarus
MEx 14
Vertical distribution of dust in the Martian atmosphere: OMEGA/MEx limb observations
DOI: 10.1016/j.icarus.2021.114702 Bibcode: 2022Icar..37114702D

Aoki, Shohei; Bellucci, Giancarlo; Altieri, Francesca +8 more

The OMEGA spectrometer on board Mars Express acquired several observations of the Martian limb that are still largely unexploited. Here, we explore the information content of these data in terms of abundance and size of the Martian atmospheric dust. We approach the dust retrievals by applying a full spherical multiple scattering Monte Carlo 1D rad…

2022 Icarus
MEx 11
Cellular patterns and dry convection in textured dust storms at the edge of Mars North Polar Cap
DOI: 10.1016/j.icarus.2022.115183 Bibcode: 2022Icar..38715183S

Sánchez-Lavega, A.; Matz, K. -D.; Tirsch, D. +9 more

We present a study of textured local dust storms that develop at the northern polar cap boundary on Mars springtime. We have used images obtained with VMC and HRSC cameras onboard Mars Express and MARCI on MRO to analyze dust storms captured from March to July 2019 (Ls = 350° in MY 34-Ls = 54° in MY 35). The textured storms grow in the longitude s…

2022 Icarus
MEx 11
The M3 project: 3 - Global abundance distribution of hydrated silicates at Mars
DOI: 10.1016/j.icarus.2021.114809 Bibcode: 2022Icar..37414809R

Poulet, François; Riu, Lucie; Carter, John

This paper is the third paper of a series that provides the modal mineralogy of the Martian surface (M3 project) at the global scale using near-infrared hyperspectral imagery. Numerous locations at the surface of Mars have previously been identified to harbor hydrated minerals which offer unique insights on the past water activity at th…

2022 Icarus
MEx 11
Late Amazonian dike-fed distributed volcanism in the Tharsis volcanic province on Mars
DOI: 10.1016/j.icarus.2022.115151 Bibcode: 2022Icar..38615151P

Pieterek, Bartosz; Lagain, Anthony; Ciazela, Marta +1 more

Tharsis is the largest volcanic province on Mars and in the solar system. This region includes major volcanoes (Olympus Mons, Alba Mons, Arsia Mons, Pavonis Mons, and Ascraeus Montes) and hundreds of small volcanic cones and vents, whose origin is not yet fully understood. Although the main Tharsis' edifices plumbing system has been extensively st…

2022 Icarus
MEx 10
Ozone vertical distribution in Mars Years 27-30 from SPICAM/MEX UV occultations
DOI: 10.1016/j.icarus.2022.115162 Bibcode: 2022Icar..38715162M

Montmessin, F.; Fedorova, A.; Korablev, O. +5 more

The SPICAM/MEX ultraviolet spectrometer probed the Martian atmosphere with the occultation method from 2004 until 2014. SPICAM/MEX performed both stellar and solar occultations during in total four Martian Years with good spatial and seasonal coverages. We have analyzed these occultations and performed a rigorous quality check of the retrievals to…

2022 Icarus
MEx 9
Presence of clay minerals can obscure spectral evidence of Mg sulfates: implications for orbital observations of Mars
DOI: 10.1016/j.icarus.2022.115083 Bibcode: 2022Icar..38315083S

Milliken, Ralph E.; Sheppard, Rachel Y.; Robertson, Kevin M.

The martian crust is often viewed through the lens of its dominant secondary minerals, Noachian phyllosilicates and Hesperian sulfates, based on orbital spectral observations. However, the effects of surface exposure on the spectra of these hydrous minerals are not fully understood. We use an environmental chamber to measure changes in near-infrar…

2022 Icarus
MEx 8
Circum-Tharsis wrinkle ridges at Lunae Planum: Morphometry, formation, and crustal implications
DOI: 10.1016/j.icarus.2021.114808 Bibcode: 2022Icar..37414808K

Karagoz, Oguzcan; Kenkmann, Thomas; Wulf, Gerwin

Wrinkle ridges are one of the most widespread tectonic landforms on Mars developed under a compressional stress regime within the lithosphere. In this study, we investigate the morphology and structure of wrinkle ridges at northern Lunae Planum, which belongs to the circum-Tharsis wrinkle ridge system. We use methods to construct balanced cross-se…

2022 Icarus
MEx 7
The lithified aeolian dune field adjacent to the Apollinaris Sulci, Mars: Geological history and paleo-wind record
DOI: 10.1016/j.icarus.2021.114788 Bibcode: 2022Icar..37314788H

Chojnacki, Matthew; Edgett, Kenneth S.; Day, Mackenzie +1 more

A lithified aeolian dune field in the Apollinaris Sulci region of Mars presents a unique opportunity to study ancient aeolian processes and paleo-wind conditions during an earlier episode of martian climate history. The ancient dunes occur inside an eroded, partly-filled impact structure. The petrified dune field retains its original geomorphology…

2022 Icarus
MEx 7