Dune Migration on Mars

A special issue of Geosciences (ISSN 2076-3263).

Deadline for manuscript submissions: closed (31 October 2021) | Viewed by 2114

Special Issue Editors


E-Mail Website
Guest Editor
Osservatorio Astronomico di Capodimonte, Istituto Nazionale di Astrofisica, 80131 Napoli, Italy
Interests: dunes; Mars; sand; wind ; migration

E-Mail Website
Guest Editor
Institute of Planetary Research, German Aerospace Center (DLR), Rutherfordstrasse 2, 12489 Berlin, Germany
Interests: geology and climate history of Mars; aeolian processes; geomorphology; spectroscopy; mineralogy; remote sensing and robotic exploration of Mars; mission operations

Special Issue Information

Dear Colleagues,

Aeolian dunes are abundant on the surface of Mars. Mostly located in a vast erg surrounding the north polar cap and inside impact craters in the Southern Martian hemisphere, dunes on Mars consist of basaltic sand and appear dark in orbiter images. Unlike Earth, where compound/complex longitudinal dunes dominate in sandy deserts, most of the dunes of Mars have a simple barchan/transverse morphology (although linear and star dune forms can also be observed), and their slopes are sculpted by large wind ripples. Despite the low density of the present-day atmosphere (six millibar on average), winds on Mars are strong enough to saltate sand and move not only ripples but even whole dune bodies. Thus, tracking the magnitude and direction of dune (and ripple) movement at the surface of Mars can give precious hints regarding surface wind circulation, sand fluxes, and erosion rates. These are key aspects when it comes to understanding the Martian geology and its atmospheric environment as meteorological data at the surface are still scarce. In addition, the movement of dunes and ripples can provide invaluable ground truth for atmospheric models.

With more than ten years of repeated high-resolution images of the surface of Mars, dune migration can now be tracked in the “long-term”, helping to address migration seasonality and the effect of extreme atmospheric events, such as dust storms. In addition, the abundance of three-dimensional surface data can help to address the complex interplay between regional/local topography and dune migration and fluxes, a topic that is still at its infancy for Mars.

This Research Topic aims to collect the latest research progress and achievements on dune migration on Mars. Contributions could include but are not limited to:

  • Using remote sensing methods in the study of dunes (and ripples) dynamics;
  • Terrestrial dune (and ripples) analogue studies;
  • Physic of sand movement;
  • CFD (computational fluid dynamics) simulations of the flow above dunes;
  • Dune mineralogy.

Dr. Simone Silvestro
Dr. Daniela Tirsch
Guest Editors

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Geosciences is an international peer-reviewed open access monthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 1800 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • dunes
  • Mars
  • sand
  • wind
  • migration

Published Papers (1 paper)

Order results
Result details
Select all
Export citation of selected articles as:

Research

14 pages, 5248 KiB  
Article
Numerical Simulations of Large Martian Impact Ripples
by Hezi Yizhaq, Jasper F. Kok, Simone Silvestro, Lior Saban and Itzhak Katra
Geosciences 2022, 12(11), 422; https://doi.org/10.3390/geosciences12110422 - 17 Nov 2022
Cited by 1 | Viewed by 1431
Abstract
Ripples made from unimodal fine sands can grow much larger on Mars than on Earth, reaching wavelengths of 1–3 m and heights exceeding 1 dm. Smaller decimeter-wavelength ripples can be superimposed on them. Classification and origins of these bedforms have been debated. They [...] Read more.
Ripples made from unimodal fine sands can grow much larger on Mars than on Earth, reaching wavelengths of 1–3 m and heights exceeding 1 dm. Smaller decimeter-wavelength ripples can be superimposed on them. Classification and origins of these bedforms have been debated. They have been interpreted as analogous to subaqueous ripples on Earth, or as aeolian impact ripples with a range of grain sizes that reach large maximum sizes on Mars. This study uses a mathematical model to evaluate the formation of large Martian ripples as aeolian impact ripples to further investigate this hypothesis. The model parameters were computed using COMSALT for 100 µm grains under shear velocity of 0.65 m/s, which is a reasonable shear velocity for sand transport on Mars according to recent estimations of threshold Martian winds. The numerical experiments utilize a large grid 8 m long. Experiments also evaluate the development of secondary small ripples between the large ripples from random perturbations. The numerical simulations show the evolution of ripple wavelength and height. According to the results, the time scale for the formation of the large ripples is about 2–3 years, which is a much longer time scale compared to terrestrial impact ripples. Small secondary ripples develop only if the space between the large ripples is sufficiently large. Full article
(This article belongs to the Special Issue Dune Migration on Mars)
Show Figures

Figure 1

Back to TopTop