Awakening Dunes
NASA/JPL/University of Arizona

Awakening Dunes
PSP_008208_2600  Science Theme: Aeolian Processes
Español  Português  


Wallpaper
800  
1024  
1152  
1280  
1440  
1600  
1920  
2048  
2560  
This image captures unusual arrow-shaped sand dunes in the north polar Olympia Undae region that may have been formed by changing winds. The dark patches and streaks show sand that has begun escaping from a blanket of seasonal frost.

Many of the typical types of Martian dunes are similar to common dunes on Earth. Transverse dunes have gentle upwind slopes and steep lee sides that are perpendicular to the wind direction. Barchans are crescent-shaped dunes with a gentle upwind slope and steep lee with horns. Other common dunes on Earth and Mars are seif dunes that form sinuous parallel ridges with bi-directional winds forming the slip-faces.

The dune types in this image transition from transverse in the south through tight chains of barchans, to the strange, elongated dunes in the north. These elongated dunes appear to be modified barchans with two slip-faces and asymmetric horns. The drawn out limbs and remnant slip-faces were apparently produced by variations in the wind direction. The winds that created the transverse dunes blow from a single easterly direction, while the modified barchans are shaped by winds from an easterly-northeasterly direction. The elongated horns align parallel to northeasterly winds. These wind variations could be caused by local topography.

Two factors likely contribute to the unique morphology of these dunes. First, the southern horns defrost sooner than the northern horns because they receive sunlight more directly. This enables material to move more easily on their southern side. Second, the changing wind directions may be reorienting the dunes. One idea is that the barchans’ southern horns are being blown downwind into linear (seif-like) dunes, with sinuous crests and steep flanks. Another possible explanation is that they are drifts of sand (lee dunes) that form in the lee of an obstacle. The frozen barchans might act as obstacles to the wind, allowing loose sand to accumulate in their lee. In either case, the interaction between the sand, wind, and seasonal frost sculpts the dunes to their unusual, arrow-like appearance.

Written by: Circe and Paul   (12 June 2008)



 Image Products: All image links are drag & drop for HiView, or click to download
JPEG
Grayscale: map projected  non-map
IRB color: map projected  non-map
RGB color: non-map projected

JP2 DOWNLOAD
Grayscale: map-projected (1328.9 MB)
IRB color: map-projected (519.2 MB)

JP2 EXTRAS
Grayscale: map-projected  (500.9 MB),
non-map  (604.8 MB)

IRB color: map projected  (152.7 MB)
non-map  (455.5 MB)


RGB color: non map-projected  (440.6 MB)
Additional Image Information
Grayscale label   Color label
Merged IRB label   Merged RGB label
EDR products

About color products (PDF)
HiView main page
HiRISE Online Image Viewer

 Observation Toolbox
Acquisition date:27 April 2008 Local Mars time: 1:51 PM
Latitude (centered):80.0 degrees Longitude (East):245.9 degrees
Range to target site:321.1 km (200.7 miles)Original image scale range:32.1 cm/pixel (with 1 x 1 binning) so objects ~96 cm across are resolved
Map projected scale:25 cm/pixelMap projection:POLAR STEREOGRAPHIC
Emission angle:7.2 degrees Phase angle:64.5 degrees
Solar incidence angle:59 degrees, with the Sun about 31 degrees above the horizon Solar longitude:64.1 degrees, Northern Spring
For non-map projected products:
North azimuth:111 degrees Sub-solar azimuth:319.1 degrees
For map-projected products
North azimuth:24.15 degreesSub solar azimuth:234.3 degrees

    Nearby observations

Usage Policy
All of the images produced by HiRISE and accessible on this site are within the public domain: there are no restrictions on their usage by anyone in the public, including news or science organizations. We do ask for a credit line where possible: Image: NASA/JPL/University of Arizona
Postscript
For information about NASA and agency programs on the Web, visit: http://www.nasa.gov. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, Calif., manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. The image data were processed using the U.S. Geological Survey’s ISIS3 software.