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Change detection and monitoring of active Martian surface phenomena with the Colour and Stereo Surface Imaging System (CaSSIS) onboard the ExoMars Trace Gas Orbiter (TGO)
DOI: 10.1016/j.icarus.2023.115443 Bibcode: 2023Icar..39415443R

Seelos, Frank P.; Tornabene, Livio L.; Osinski, Gordon R. +10 more

Mars is host to a variety of active surface processes that relate to changes in seasonal ice/frost, slope activity, wind and processes potentially relating to liquid water. Regular monitoring and change detection of these phenomena is crucial to not only provide us insights into present day Martian surface conditions, but also its past geologic an…

2023 Icarus
ExoMars-16 4
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
Dendritic ridges in Antoniadi basin, Mars: Fluvial or volcanic landforms?
DOI: 10.1016/j.icarus.2023.115735 Bibcode: 2023Icar..40615735M

Mangold, N.; Thomas, N.; Hauber, E. +7 more

Antoniadi basin displays dark-toned dendritic ridges previously interpreted as inverted fluvial channels. Detailed observations of these dark-toned ridges as well as the geological units in the central region of Antoniadi basin are provided emphasizing images from the Colour and Stereo Surface Imaging System (CaSSIS), the High Resolution Stereo Ca…

2023 Icarus
ExoMars-16 MEx 0