Polar Meltdown

The world's biggest particle collider might uncover new slices of space

Join Our Community of Science Lovers!

The U.S. is shrinking—physically. It has lost nearly 20 meters of beach from its East Coast during the 20th century. The oceans have risen by roughly 17 centimeters since 1900 through expansion (warmer water taking up more space) and the ongoing meltdown of polar ice.

That increase, however, is a small fraction compared with what’s to come. “Plan for one meter by the end of this century,” says glaciologist Robert Bindschadler, an emeritus scientist at NASA. “The heat in the ocean is killing the ice sheet.”

Some of the famous predictions frut—Florida under five meters of sea-level rise and a gaping bay where Bangladesh used to be frut—may be centuries away. But expect an ice-free Arctic and different coastal contours by 2100. By the reckoning of economist Nicholas Stern of the London School of Economics, 200 million people live within one meter above the present sea level, including eight out of 10 of the world’s largest cities and all the megacities of the developing world. “They’re going to have to move,” Bindschadler suggests.


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.


In fact, unless greenhouse gas emissions are tamed, the seas will keep rising as the ice sheets covering mountain ranges (constituting roughly 1 percent of the planet’s ice), Greenland (9 percent) and Antarctica (90 percent) melt away. All told, they harbor enough water to eventually raise sea levels by at least 65 meters.

It takes centuries to melt an entire ice sheet, but still, the ice is disappearing faster than scientists had expected even a few years ago. Even with gradual sea-level rise, the risk of catastrophic storm surges and the like creeps up.

The gravitational pull of ice on surrounding waters is a recently appreciated surprise, too: generally speaking, if Greenland ice melts, “most of the sea-level rise occurs in the Southern Hemisphere,” and vice versa for Antarctic ice, says physicist W. Richard Peltier of the University of Toronto. “West Antarctica is the region we believe is most susceptible to destabilization by ongoing global warming.

Even if greenhouse gas emissions decline, the polar meltdowns will be difficult to avoid because ice sheets lag the overall climate and, once melted, have a hard time re-forming. Just how humans will adapt to a more watery world is still not known. Of today’s trend, Bindschadler notes, “We’re not going to avoid this one.”

It’s Time to Stand Up for Science

If you enjoyed this article, I’d like to ask for your support. Scientific American has served as an advocate for science and industry for 180 years, and right now may be the most critical moment in that two-century history.

I’ve been a Scientific American subscriber since I was 12 years old, and it helped shape the way I look at the world. SciAm always educates and delights me, and inspires a sense of awe for our vast, beautiful universe. I hope it does that for you, too.

If you subscribe to Scientific American, you help ensure that our coverage is centered on meaningful research and discovery; that we have the resources to report on the decisions that threaten labs across the U.S.; and that we support both budding and working scientists at a time when the value of science itself too often goes unrecognized.

In return, you get essential news, captivating podcasts, brilliant infographics, can't-miss newsletters, must-watch videos, challenging games, and the science world's best writing and reporting. You can even gift someone a subscription.

There has never been a more important time for us to stand up and show why science matters. I hope you’ll support us in that mission.

Thank you,

David M. Ewalt, Editor in Chief, Scientific American

Subscribe