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Mars south polar region Fenton & Hayward (2010) |
Operating between 1.8 and 5mhz, MARSIS reflects 10W radio waves off the surface at a repetition frequency of 127.7 hz. Water has a unique higher reflection property than the surface. With multiple passes by the orbiter, the surface area of interest can get scanned at slightly different regions revealing a region that indicates the potential of a pond or lake. The researchers used data gathered from 2010 to 2019 from MARSIS to strengthen the overall evidence.
Described as lakes and ponds, the water is most likely a slush-like, high saline solution that is pooled about 1 mile under the surface with a temperature of about -90F.
Though it is still too early to fully confirm the discovery of subglacial lakes, this is mounting evidence that should help drive more missions that can eventually use water to fuel hydrogen for Martian bases and/or missions.
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