Multi-year measurements of ripple and dune migration on Mars: Implications for the wind regime and sand transport
Abstract
Aeolian sand dunes are observed across the Martian surface. The arrival of the HiRISE camera on Mars Reconnaissance Orbiter at Mars in 2006 enabled detection of modern-day movement of dunes and ripples from orbit for the first time. Since 2006, HiRISE collected a long timeseries of repeat imagery at a few Martian dune fields. We analyze this timeseries of imagery at two of these dune fields, using COSI-Corr for image registration and correlation, to study the movement and dynamics of dunes and meter-scale ripples at the Nili Patera and Meroe Patera barchan dune fields. We present measurements of whole-dune translational sand fluxes extracted at both dune fields via manual tracking of dune crestlines and slipfaces in HiRISE images. We also present a multi-Mars year timeseries of ripple flux measurements. Ripple migration shows a consistent pattern of seasonal variation, with maxima in flux during northern-hemisphere autumn and winter at both dune fields. Ripple migration is also observed to decrease away from the upwind margins of dune fields. We compare our observations with predicted sand transport using winds output from the MarsWRF atmospheric circulation model and theories of sand motion. The model predicts half-hourly, mesoscale winds, from which we estimate the 1 Hz, local-scale winds by assuming a Weibull distribution of wind speed, with parameters chosen based on landed wind data. This approach uses remote sensing observations of bedform migration, and comparisons with model output, to place constraints on the wind regime. Our measurements of the seasonal pattern of sand flux variation agree, to first order, with predictions based on modeled wind speeds. Comparison of the magnitudes of predicted and observed sand fluxes is not feasible due to the high uncertainties in our calculated sand fluxes caused by uncertainties in input parameters, most importantly the assumed fluid threshold for sand transport. However, we note that model predictions fit our observed sand fluxes best when relatively low values of the fluid threshold shear velocity of ~0.6–0.8 m/s (or shear stresses of O(10−3) Pa) are assumed.
Copyright and License
© 2022 Published by Elsevier Inc.
Acknowledgement
This work was supported by funding from the King Abdulaziz City for Science and Technology, and from NASA Grant NNX16AJ43G/123117. We also thank Drs. Joel Davis and Thomas Pähtz for their reviews which helped improve this manuscript.
Funding
This work was supported by funding from the King Abdulaziz City for Science and Technology, and from NASA Grant NNX16AJ43G/123117.
Supplemental Material
Supplementary material: In all movies, depicting results from the MarsWRF climate model,lines of longitude and latitude are shown by values on the X and Y axis. Background color is by elevation. The Nili Patera dune field’s location is marked with a blue ‘X’, while Meroe Patera is marked with a yellow ‘X’. Movies S2-S5 are domain 2 simulations, while Movies S6-S9 are higher resolution domain 3 simulations.
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Additional details
- King Abdulaziz City for Science and Technology
- National Aeronautics and Space Administration
- NNX16AJ43G/123117
- Accepted
-
2022-02-21Accepted
- Accepted
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2022-02-26Available online
- Available
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2022-03-21Version of record
- Caltech groups
- Division of Geological and Planetary Sciences, Seismological Laboratory
- Publication Status
- Published