Distribution and Morphologies of Transverse Aeolian Ridges in ExoMars 2020 Rover Landing Site
Metadatos
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MDPI
Materia
Transverse aeolian ridge (TAR) ExoMars 2020 Oxia Planum Mapping
Fecha
2019-04-15Referencia bibliográfica
Bhardwaj, A., Sam, L., Martin-Torres, F. J., & Zorzano, M. P. (2019). Distribution and Morphologies of Transverse Aeolian Ridges in ExoMars 2020 Rover Landing Site. Remote Sensing, 11(8), 912.
Resumen
Aeolian processes are believed to play a major role in the landscape evolution of Mars.
Investigations on Martian aeolian landforms such as ripples, transverse aeolian ridges (TARs),
and dunes, and aeolian sediment flux measurements are important to enhance our understanding
of past and present wind regimes, the ongoing dust cycle, landscape evolution, and geochemistry.
These aeolian bedforms are often comprised of loose sand and sharply undulating topography and
thus pose a threat to mobility and maneuvers of Mars rovers. Here we present a first-hand account of
the distribution, morphologies, and morphometrics of TARs in Oxia Planum, the recently selected
ExoMars 2020 Rover landing site. The gridded mapping was performed for contiguous stretches of
TARs within all the landing ellipses using 57 sub-meter high resolution imaging science experiment
(HiRISE) scenes. We also provide the morphological descriptions for all types of TARs present within
the landing ellipses. We use HiRISE digital terrain models (DTMs) along with the images to derive
morphometric information for TARs in Oxia Planum. In general, the average areal TAR coverage
was found to be 5.4% (+/-4.9% standard deviation), increasing from west to east within the landing
ellipses. We report the average TAR morphometrics in the form of crest–ridge width (131.1 +/- 106.2 m),
down-wind TAR length (17.6 +/- 10.1 m), wavelength (37.3 +/- 11.6 m), plan view aspect ratio (7.1 +/- 2.3),
inter-bedform spacing (2.1 +/- 1.1), slope (10.6º +/- 6.1º), predominant orientations (NE-SW and E-W),
and height (1.2 +/- 0.8 m). While simple TARs are predominant, we report other TAR morphologies such
as forked TAR, wavy TAR with associated smaller secondary ripples, barchan-like TAR, networked
TAR, and mini-TARs from the region. Our results can help in planning the rover traverses in terms
of both safe passage and scientific returns favoring aeolian research, particularly improving our
understanding of TARs.