Seasonal Erosion and Restoration of Mars' Northern Polar Dunes

• Autor: Hansen, C. J. ; Bourke, M. ; Bridges, N. T. ; Byrne, S. ; Colon, C. ; Diniega, S. ; Dundas, C. ; Herkenhoff, K. ; McEwen, A. ; Mellon, M. ; Portyankina, G. ; Thomas, N.
• Assuntos: Aprons ; Carbon Dioxide ; Cosmochemistry. Extraterrestrial geology ; Dry Ice ; Dunes ; Earth sciences ; Earth, ocean, space ; Erosion ; Exact sciences and technology ; Extraterrestrial Environment ; Extraterrestrial geology ; Gullies ; Ice ; Imaging ; Mars ; Planetary science ; Planetology ; Polar regions ; Restoration ; Ripples ; Sand ; Sand & gravel ; Science Experiments ; Sediment transport ; Sediments
• É parte de: Science (American Association for the Advancement of Science), 2011-02, Vol.331 (6017), p.575-578
• Notas: ObjectType-Article-1
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• Descrição: Despite radically different environmental conditions, terrestrial and martian dunes bear a strong resemblance, indicating that the basic processes of saltation and grainfall (sand avalanching down the dune slipface) operate on both worlds. Here, we show that martian dunes are subject to an additional modification process not found on Earth: springtime sublimation of Mars' CO₂ seasonal polar caps. Numerous dunes in Mars' north polar region have experienced morphological changes within a Mars year, detected in images acquired by the High-Resolution Imaging Science Experiment on the Mars Reconnaissance Orbiter. Dunes show new alcoves, gullies, and dune apron extension. This is followed by remobilization of the fresh deposits by the wind, forming ripples and erasing gullies. The widespread nature of these rapid changes, and the pristine appearance of most dunes in the area, implicates active sand transport in the vast polar erg in Mars' current climate.
  
• Editor: Washington, DC: American Association for the Advancement of Science
  
• Idioma: Inglês