CaltechAUTHORS
  A Caltech Library Service

High Sand Fluxes and Abrasion Rates on Mars Determined from HiRISE Images

Bridges, N. T. and Ayoub, F. and Avouac, J.-P. and Leprince, S. and Lucas, A. and Mattson, S. (2012) High Sand Fluxes and Abrasion Rates on Mars Determined from HiRISE Images. In: 43rd Lunar and Planetary Science Conference, March 19-23, 2012, The Woodlands, TX. http://resolver.caltech.edu/CaltechAUTHORS:20160318-162107096

[img] PDF - Published Version
See Usage Policy.

132Kb

Use this Persistent URL to link to this item: http://resolver.caltech.edu/CaltechAUTHORS:20160318-162107096

Abstract

The volumetric transport rate of sand, or flux, is a fundamental parameter that controls the rate of landscape modification. This process is responsible for the movement of ripples and dunes, as well as the abrasion of rocks and landforms. Measuring sand flux on Mars was previously not possible because of the lack of high spatial and temporal resolution images, and appropriate techniques, for making displacement and accurate topographic measurements. These limitations have now been overcome because, 1) It is found that many dunes and ripples on Mars are mobile in High Resolution Imaging Science Experiment (HiRISE) images [1-4], and 2) the application of precise image registration and correlation methods permits the quantification of movement to sub-pixel precision that, when combined with topographic data, can be used to derive the sand flux. Sand transport occurs via two modes, saltation and reptation [5,6]. Saltation occurs in long hops initiated from aerodynamic shear and subsequent propagation as grains are rebounded or ejected downstream. Reptation operates via shorter hops resulting from the “splash” ejection induced by the collision of upwind saltating grains. Reptation contributes to the migration of ripples whereas both processes result in the net movement of dunes. Therefore, by knowing the rate of movement of these bedforms and their volume, the reptation and saltation flux can be estimated. Here, we measure the migration rate of sand ripples and dune lee fronts at Nili Patera, Mars. From these data, we derive the reptation and total (reptation + saltation) fluxes, respectively. The dunes have unexpectedly high sand fluxes that are like those in Victoria Valley, Antarctica, implying that rates of landscape modification on Mars and Earth are similar.


Item Type:Conference or Workshop Item (Paper)
Related URLs:
URLURL TypeDescription
http://www.lpi.usra.edu/meetings/lpsc2012/pdf/1322.pdfPublisherPaper
ORCID:
AuthorORCID
Avouac, J.-P.0000-0002-3060-8442
Group:Keck Institute for Space Studies
Record Number:CaltechAUTHORS:20160318-162107096
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20160318-162107096
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:65496
Collection:CaltechAUTHORS
Deposited By: Colette Connor
Deposited On:18 Mar 2016 23:41
Last Modified:18 Mar 2016 23:41

Repository Staff Only: item control page