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The frozen mountains and icy plains of Antarctica hold enough water to raise global sea levels nearly 200 feet. Thankfully, over three-quarters of the continent is girded by ice shelves, the floating extensions of glaciers that protect the land-bound ice behind them like walls surrounding a vast, icy castle. But scientists are discovering new vulnerabilities that could weaken those walls from above and below.
In the frigid realm of East Antarctica, tens of thousands of brilliant blue lakes are forming across ice shelves in the summertime—far more than scientists previously realized, according to a study published last month in Scientific Reports. Meanwhile, in rapidly-melting parts of West Antarctica, “upside down rivers” of warm water are gnawing away at the ice shelves’ weak spots from below, according to a study published Wednesday in Science Advances.
As the Earth continues to warm, both processes could hasten the demise of Antarctica’s icy armor and the giant glaciers it holds back.
Invasion of the blue lakes
For much of the year, the ice blanketing Earth’s polar regions is locked in a deep freeze. But on mild summer days, the surface of the ice begins to melt, draining into depressions and forming topaz blue lakes.
Beautiful as they are, these lakes are bad news for ice. Because of their dark color, they absorb more of the sun’s energy, triggering further warming. And under certain conditions, clusters of lakes can drain rapidly into the ice below them, causing it to break apart in a process known as “lake-induced hydrofracturing.”
scientists have been intensively studying these meltwater lakes across fast-warming parts of Greenland and the Antarctic Peninsula. Now, a team of researchers has conducted the first systematic survey of meltwater lakes in East Antarctica, the coldest part of the continent and home to its most stable ice.
The study only looked at one melt season, and a weird one at that: In late 2016 and early 2017, mild weather and unusual atmospheric circulation patterns gripped Antarctica’s coastlines, causing its sea ice to crash. The scientists are planning to repeat their analysis with additional years of satellite data, Stokes said. But even if 2017 was an outlier, the study suggests some of East Antarctica's ice shelves could be more vulnerable to warm years than we thought.
Upside-down Rivers
As lakes raise concerns about the future of East Antarctica’s ice shelves, to the west an unseen force is attacking ice from below. Blobs of warm water are rising up from the deep, forming river-like channels that eat away at the bottoms of those ice shelves.
Several years back, Karen Alley, a glaciologist at the College of Wooster, began studying these ‘upside down rivers’ via satellite imagery. By examining depressions at the surface of the ice, she could tell that some of them were enormous—up to three miles wide, tens of miles long, and hundreds of feet deep. She also noticed that the rivers frequently formed below what glaciologists call “shear margins,” weak points at the edges of ice shelves.
In their latest research, Alley and her co-authors used satellite imagery to try and understand why that is. As they report in their new paper, the formation of rivers beneath shear margins seems to start on the land, when flowing ice streams are stretched and thinned along their edges. When those stretch zones reach the ocean, they rise up relative to the thicker ice surrounding them, creating what looks like an inverted river bed running across the bottom of the shelf. Rising warm water gets funneled into that bed, forming an upside down river.
The researchers found that the rivers are most likely to form beneath fast-flowing ice, including the ice shelves protecting West Antarctica’s imperiled Pine Island and Thwaites glaciers. “There were a lot more of these ice shelf channels on shear margins than we thought,” Alley says.
originally posted by: Athetos
(pretty short amount of time on the scale we are dealing with here.)
originally posted by: LtFluffyCakes96
originally posted by: Athetos
(pretty short amount of time on the scale we are dealing with here.)
And we could very well be shortening that amount of time even more.
a heavily forested area that became iced over in a few hundred years
At the beginning of the Oligocene Epoch, some 33 million years ago, the South Pole – Antarctica – went from being largely forested – a little like New Zealand, say, to being largely ice-bound in a mere few hundred thousand years.
originally posted by: KansasGirl
What the heck is an "upside down river?" Can anyone help me visualize that?
Buoyant plumes of warm ocean water beneath ice shelves can be focused into these basal troughs, localizing melting and weakening the ice-shelf margins.
originally posted by: CthruU
originally posted by: LtFluffyCakes96
originally posted by: Athetos
(pretty short amount of time on the scale we are dealing with here.)
And we could very well be shortening that amount of time even more.
Ahh I see now, this thread is another angle on climate change caused by humans.
But -
Judging by the elites that have transited down there the last few years they've clearly found alot more than just upside down lakes and hidden rivers.
originally posted by: MrConspiracy
The planet changes. We should do what we can to not accelerate these changes but people must understand we can't "save" the planet. Regardless of our existence, the climate changes.
The world has been hotter than this. The world has been cooler than this.
If we are so accountable, why have things been worse without us?
originally posted by: hopenotfeariswhatweneed
originally posted by: MrConspiracy
The planet changes. We should do what we can to not accelerate these changes but people must understand we can't "save" the planet. Regardless of our existence, the climate changes.
The world has been hotter than this. The world has been cooler than this.
If we are so accountable, why have things been worse without us?
What matters is our ability to thrive, luckily we humans are adaptable.