Antarctica’s meltwater rivers raise concerns about the fate of the continent | RenewEconomy

Antarctica’s meltwater rivers raise concerns about the fate of the continent

When climate scientists look at Antarctica, they see a ticking time bomb. If the ice sheet melts, sea levels will rise dramatically.


Nexus Media

When climate scientists look at Antarctica, they see a ticking time bomb. If the ice sheet melts, it will raise sea levels by tens of metres, flooding coastal cities around the globe.

For now, the southern continent is relatively stable, but it’s starting to look more like Greenland, where rising temperatures are melting the island from the inside out.

For decades, Greenland primarily melted around the edges. Giant blocks of ice would break free from the coast and vanish into the ocean. Recently, however, Greenland has started melting from the middle. Pools of water are forming atop the ice sheet in the warmer months and then draining out to sea.

Scientists have now discovered the same thing is happening in Antarctica. Two new studies published in the journal Nature catalogue the melting and explain what it could mean for sea-level rise.

In the first study, researchers examined decades of photos from satellites and military aircraft. They documented hundreds of meltwater channels around the perimeter of the continent. They traced some streams deep into Antarctica’s frozen interior and discovered ponds of meltwater more than 4,000 feet above sea level, where no one expected to find liquid H2O.

In some places, the terrain had contributed to the melting. Blue ice and dark mountains absorb more sunlight than the white snow. These features gathered extra heat needed to thaw Antarctic ice.

Exposed rock and blue ice absorb sunlight, accelerating melting.
Exposed rock and blue ice absorb sunlight, accelerating melting.

“Even though people kind of knew there were melt ponds around, they really didn’t know that water could move long distances across the surface,” said Jonathan Kingslake, a glaciologist at Columbia University and lead author of the study. He said that streams “take water away from the surface of the ice sheet and actually export it all the way into the ocean… And we didn’t really realize this happened at all.”

Meltwater channels tend to grow in warmer months and refreeze in the winter. But scientists worry that rising temperatures spur continual melting, accelerating sea-level rise.

Ice shelves along the edge of the continent are holding back massive, terrestrial glaciers. As the shelves break up, they allow glaciers to slip into the ocean. Meltwater will burrow into the ice shelf, cleaving apart large chunks of ice. (That’s what’s happening to the Larsen C Ice Shelf, which is expected to break off the continent soon.) Meltwater can also lubricate the underside of the glacier, hastening its passage to the sea.

When ice shelves disintegrate, glaciers move out to sea.
When ice shelves disintegrate, glaciers move out to sea.

Kingslake said the drainage systems appear “quite stable at the moment. But the predictions for the future — for this century — are that melt rates will double in response to global climate change.” He said that “what we really need to know is how is that going to impact the stability of the ice sheet and our predictions of sea-level rise.”

The second study, which Kingslake co-authored, attempts to answer that question.

“When we turn the temperature up — of the atmosphere — we’re going to make more melt, and it’s going to get caught in ponds, and it’s going to act like a jackhammer and ruin the ice shelf,” said Robin Bell, a geophysicist at Columbia University, lead author of the second study and co-author of the first.

But, Bell said there are signs of hope. She noted that meltwater channels have kept West Antarctica’s Nansen Ice Shelf intact. That’s because water is draining to the ocean rather than amassing on the surface, where it would warm up the ice and trigger further melting.

nansen ice shelf
The Nansen Ice Shelf.

“Plumbing on our planet matters, and plumbing on the top of the ice sheet matters,” said Bell. The water on the Nansen Ice Shelf isn’t gathering into pools or “falling into these crevices that then pop open. Instead, it’s exiting stage right down this very subtle river valley.” The runoff has a negligible effect on sea levels.

Antarctica is contributing to sea-level rise in other ways, shedding chunks of ice around the edges. Between 2002 and 2016, Antarctica shed 100 gigatonsof ice per year — nearly enough water to fill Lake Ontario. Antarctica — like Greenland — is less stable than previously thought. Recent research suggests climate change could raise sea levels by six feet by the end of this century, and by tens or even hundreds of feet in the centuries to come. New research on meltwater complicates scientists’ projections.

Antarctica lost 100 gigatons of ice per year between 2002 and 2016
Antarctica lost 100 gigatons of ice per year between 2002 and 2016

“We’re working hard to figure out if this stuff is relevant to sea-level predictions,” said Douglas MacAyeal, a glaciologist at the University of Chicago who was not involved in the studies. He noted that, until recently, “nobody’s been that interested in melting,” because it was thought to be extremely rare in Antarctica.

Scientists will need to better understand the inner workings of the Antarctic ice sheet to forecast sea levels in the decades to come. What happens on the southern continent rarely stays there. Melting glaciers threaten to deliver floods to New Orleans, Miami, New York and beyond.

“This might delay how fast the other parts of Antarctica go,” said Bell, “but it doesn’t mean that Antarctica isn’t susceptible to changing temperatures.”

 Jeremy Deaton, Josh Chamot and Owen Agnew write and produce videos for Nexus Media, a syndicated newswire covering climate, energy, policy, art and culture.

Source: Nexus Media. Reproduced with permission.

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  1. D. John Hunwick 4 years ago

    Sea level rise is real. Every year new forecasts as to the amount it will rise by 2100 increases. The latest New Scientist says 3 metres. I prefer to think that James Hansen’s prediction of 5 metres by 2050 will be much closer to the mark. Yet no one seems to realise that this process is unstoppable. Slow yes but also inexorable. The time for action is now, not in 2050 or 2075. What to do? A short list says: use only renewable energy at home and at work, save up for a fully electric vehicle, get energy storage, invest any money possible into ethical banking, get your super fund to do the same. Who knows when it will be too late for even these things to be effective??

    • Mike Dill 4 years ago

      If every use of fossil fuel stops right now, the three meters of sea level rise that the New Scientist forecasts will happen. Unfortunately, I also think that the 5 meter prediction will come to pass, but probably not as soon as James Hanson thinks.

      • D. John Hunwick 4 years ago

        Thank you for your sensible response. It hurts me to think that a 3m rise is inevitable and no-one seems to really care at what we will lose.

        • solarguy 4 years ago

          I care John, very much so in fact. I too share you concerns and frustrations. Our planet can achieve 100% renewable energy or close to it by 2050, it simply is a must do scenario.
          I’m doing my part, my home is completely off grid currently until I can sort out inverter settings that will allow me to sell my excess solar to the grid.

          • D. John Hunwick 4 years ago

            I am following the same route as yourself. Does change to 100% renewable really depend on people like us to achieve it – or is there another way?

          • solarguy 4 years ago

            The main reason that we are going to renewables now in a big way is that solar and wind and storage are cheaper than fossil fuels. I think if it was only up to people like ourselves, probably not.
            Damn good luck for the planet that money is the ironic saviour.

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