New Issue: Orbital Catastrophe Ahead? Read Now

Martian Glaciers Equal Meter-Thick Planetary Ice Shell

Radar measurements and models of Earthly glacial ice flows led researchers to conclude that the glaciers spotted on Mars from orbiters contain nearly 150 billion cubic meters of water. Lee Billings reports   

 

Illustration of a Bohr atom model spinning around the words Science Quickly with various science and medicine related icons around the text

Join Our Community of Science Lovers!


On supporting science journalism

If you're enjoying this article, consider supporting our award-winning journalism by subscribing. By purchasing a subscription you are helping to ensure the future of impactful stories about the discoveries and ideas shaping our world today.


Long before the space age, humans looking at Mars thought they saw evidence for the presence of water, in the form of giant canals built by some very advanced, very thirsty civilization. Those 19th-century notions proved to be the products of poor telescopes and wishful thinking—the canals were an optical illusion. But 20th- and 21st-century observers have definitely found water on Mars.
 
Telescopes spied water in ice caps at the Red Planet’s poles, as well as signs of an ancient ocean covering the northern hemisphere. The Viking landers saw water frost on rocks, the Phoenix lander found water ice buried centimeters beneath the soil, and the Curiosity rover has rolled through an ancient riverbed.

Most mysteriously, orbiters overhead have glimpsed the outlines of what seem to be belts of buried glaciers girdling the globe at high latitudes. Some researchers thought the dust-covered glaciers might be mostly made of mud, or of carbon dioxide ice. But a new study from researchers at the University of Copenhagen reinforces the consensus view that the glaciers are made of water ice—and a lot of it. The findings are in the journal Geophysical Research Letters. [N. B. Karlsson, L. S. Schmidt and C. S. Hvidbert, Volume of Martian mid-latitude glaciers from radar observations and ice-flow modeling]

The researchers paired a decade’s worth of radar measurements with models of how glacial ice flows on Earth to calculate the approximate thickness and size of all the Martian glaciers.
 
Their conclusions? The glaciers contain nearly 150 billion cubic meters of water ice—enough ice to cover Mars a meter deep, and more than enough to someday sustain human colonists. Though of course they’d need to find a way to melt and move all that water around. Who knows—maybe they’d build canals.
 
—Lee Billings
 
[The above text is a transcript of this podcast.]
 

Lee Billings is a science journalist specializing in astronomy, physics, planetary science, and spaceflight and is senior desk for physical science at Scientific American. He is author of a critically acclaimed book, Five Billion Years of Solitude: The Search for Life Among the Stars, which in 2014 won a Science Communication Award from the American Institute of Physics. In addition to his work for Scientific American, Billings’s writing has appeared in the New York Times, the Wall Street Journal, the Boston Globe, Wired, New Scientist, Popular Science and many other publications. Billings joined Scientific American in 2014 and previously worked as a staff editor at SEED magazine. He holds a B.A. in journalism from the University of Minnesota.

More by Lee Billings

Subscribe to Support Independent Journalism

Great science journalism requires human expertise, time, effort and creativity. And it costs money. That’s why I and the journalists here at Scientific American hope you’ll join our community.

When you subscribe, you are supporting staff and freelance journalists who are passionate about telling science stories that are true, important and compelling. Our editors and reporters are often experts in their fields, which means they understand the nuances of big discoveries and can untangle the breakthroughs from the hype. With a subscription, you are also supporting rigorous fact-checking to ensure the words we publish are precise and accurate. And you’re supporting original illustrations, graphics and photos that bring you closer to an advanced laboratory, an ice sheet in Antarctica or a space mission in orbit. You’re helping us craft other types of high-quality journalism as well: Our newsletters are carefully written, edited and curated by staffers you have or will come to know and love. Our Science Quickly podcast is based on original reporting, collaboration with editors and scientists and exacting production.

Subscriptions keep this engine running so we can continue to deliver thoughtful, rigorous and independent science journalism to you. In an era of viral misinformation, this work is crucial. If you value what we do, I hope you’ll consider joining us as a subscriber

Thank you,

Jeanna Bryner, Editor in Chief, Scientific American

Subscribe