{"id":195643,"date":"2025-11-23T07:44:15","date_gmt":"2025-11-23T07:44:15","guid":{"rendered":"https:\/\/www.europesays.com\/ie\/195643\/"},"modified":"2025-11-23T07:44:15","modified_gmt":"2025-11-23T07:44:15","slug":"maybe-thats-not-liquid-water-on-mars-after-all","status":"publish","type":"post","link":"https:\/\/www.europesays.com\/ie\/195643\/","title":{"rendered":"Maybe That\u2019s Not Liquid Water on Mars After All"},"content":{"rendered":"

Source: Geophysical Research Letters<\/a><\/p>\n

Ancient Mars<\/a> boasted abundant water, but the cold and dry conditions of today make liquid water on the Red Planet seem far less probable. However, the Mars Advanced Radar for Subsurface and Ionosphere Sounding (MARSIS<\/a>) detected<\/a> strong radar reflections from a 20-kilometer-wide area over the base of Mars\u2019s southern polar ice cap, hinting at the possibility of liquid water below the icy surface. Such a finding would have major implications for the planet\u2019s possible habitability.<\/p>\n

But sustaining liquid water underneath the ice might not be feasible without very salty brines or localized volcanic heat. Scientists have deliberated about other possible \u201cdry\u201d explanations for the bright reflections detected by MARSIS, such as layers of carbon dioxide and water ices or salty ice and clay causing elevated radar reflectivity.<\/p>\n

Aboard the Mars Reconnaissance Orbiter<\/a>, the Shallow Radar (SHARAD<\/a>) uses higher frequencies than MARSIS. Until recently, though, SHARAD\u2019s signals couldn\u2019t reach deep enough into Mars to bounce off the base layer of the ice where the potential water lies\u2014meaning its results couldn\u2019t be compared with those from MARSIS.<\/p>\n

However, the Mars Reconnaissance Orbiter team recently tested a new maneuver that rolls the spacecraft on its flight axis by 120\u00b0\u2014whereas it previously could roll only up to 28\u00b0<\/a>. The new maneuver, termed a \u201cvery large roll,\u201d<\/a> or VLR, can increase SHARAD\u2019s signal strength and penetration depth, allowing researchers to examine the base of the ice in the enigmatic high-reflectivity zone.<\/p>\n

Morgan et al.<\/a> examined 91 SHARAD observations that crossed the high-reflectivity zone. Only when using the VLR maneuver was a SHARAD basal echo detected at the site. In contrast to the MARSIS detection, the SHARAD detection was very weak, meaning it is unlikely that liquid water is present in the high-reflectivity zone. The researchers suggest that the faint detection returned by SHARAD under this portion of the ice cap is likely due to a localized region of smooth ground beneath the ice. They add that further research is needed to reconcile the differences between the MARSIS and SHARAD findings. (Geophysical Research Letters, https:\/\/doi.org\/10.1029\/2025GL118537<\/a>, 2025)<\/p>\n

\u2014Rebecca Owen (@beccapox.bsky.social<\/a>), Science Writer<\/p>\n

\"A<\/a><\/p>\n

Citation:<\/strong>\u00a0Owen, R. (2025), Maybe that\u2019s not liquid water on Mars after all,\u00a0Eos, 106, https:\/\/doi.org\/10.1029\/2025EO250437. Published on 21 November 2025.<\/p>\n

Text \u00a9 2025. AGU.\u00a0CC BY-NC-ND 3.0<\/a>
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.<\/p>\n

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