A new study, led by the University of Cambridge, has uncovered further evidence suggesting there could be liquid water on Mars. It is said to provide the first independent line of evidence using data other than radar to show liquid water beneath Mars’ south polar ice cap.
However, this “does not necessarily mean that life exists on Mars”, the experts stressed. The international research team included scientists from the University of Sheffield and the Open University, as well as counterparts from the University of Nantes and University College Dublin.
Like Earth, Mars has thick water ice caps at both poles, with their combined volume roughly equivalent to the Greenland Ice Sheet. While Earth’s ice sheets are underlain by water-filled channels and subglacial lakes, it was previously thought that those on Mars were frozen solid all the way to their beds due to the cold Martian climate.
Spacecraft laser-altimeter measurements of the shape of the upper surface of the ice were used to identify subtle patterns in its height. These patterns were then shown to match computer model predictions for how a body of water beneath the ice cap would affect the surface.
The findings matched with previous ice-penetrating radar measurements that were originally interpreted to show a potential area of liquid water beneath the ice.
Dr Frances Butcher, second author of the study from the University of Sheffield, said: “This study gives the best indication yet that there is liquid water on Mars today because it means that two of the key pieces of evidence we would look for when searching for subglacial lakes on Earth have now been found on Mars. Liquid water is an essential ingredient for life, although it does not necessarily mean that life exists on Mars.
“In order to be liquid at such cold temperatures, the water beneath the south pole might need to be really salty, which would make it difficult for any microbial life to inhabit it. However, it does give hope that there were more habitable environments in the past when the climate was less unforgiving.”
Professor Neil Arnold, from Cambridge’s Scott Polar Research Institute, led the research and added: “The combination of the new topographic evidence, our computer model results and the radar data make it much more likely that at least one area of subglacial liquid water exists on Mars today, and that Mars must still be geothermally active in order to keep the water beneath the ice cap liquid.”
