Water in Alaska sand dunes hints at wetter Mars
The presence of liquid water at and beneath frozen Alaskan sand dunes during the winter months suggests that liquid water could also be temporarily stable (or metastable) at frost-covered sand dunes on Mars.
A team of Earth and planetary scientists from Southwest Research Institute (SwRI) performed field studies of the Great Kobuk Sand Dunes, which serve as an Earth-based cold-climate “analog” to dunes on the Red Planet.
The team conducted fieldwork in Kobuk Valley National Park, Alaska, when the average daily surface temperature was -14.7°C. Geophysical data gathered by SwRI scientists strongly suggest that there is a perched layer of liquid water in the dunes occurring just below the seasonally frozen active layer.
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