Asteroid Impacts Could Have Warmed Ancient Mars
Mars is a frigid world today, and all of its surface water is frozen solid. However, there’s ample evidence that liquid water once coursed over the Red Planet. That paradox has sparked an ongoing debate: What warmed up Mars’s climate billions of years ago? A team now has proposed that giant asteroid impacts—the kinds that carve out basins exceeding 1,200 kilometers in diameter—might have played an important role. In a process known as oxidation, iron-bearing minerals reacted with water present in Mars’s subsurface to produce iron oxides and hydrogen gas. That hydrogen then went on to collide with the carbon dioxide already present in Mars’s atmosphere. All of that bumping together of molecules changes their electronic structure and allows them to absorb radiation at a wider range of wavelengths, an experimentally verified phenomenon known as collision-induced absorption. “These molecules become even better greenhouse gases,” said Ramses Ramirez, a planetary scientist at the University of Central Florida in Orlando not involved in the research. Recent research has suggested that an atmosphere composed of both carbon dioxide and hydrogen can reach temperatures above freezing. On the other hand, a carbon dioxide–dominated atmosphere void of hydrogen or other greenhouse gases can attain a top temperature of only about −40°C, Ramirez said. “That’s over 40° too cold.”
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