A
Giant, Mysterious Hole Has Opened Up in Antarctica
“We’re
still trying to figure out what’s going on.”
11
October, 2017
A
hole as large as Lake Superior or the state of Maine has opened up in
Antarctica, and scientists aren't sure why it's there.
The
gigantic, mysterious hole "is quite remarkable,"
atmospheric physicist Kent
Moore,
a professor at the University of Toronto's Mississauga campus, told
me over the phone. "It looks like you just punched a hole in the
ice."
;"
An
image of the hole in the sea ice. Image: MODIS-Aqua via NASA
Worldview; sea ice contours from AMSR2 ASI via University of Bremen
Areas
of open water surrounded by sea ice, such as this one, are known
as polynias.
They form in coastal regions of Antarctica, Moore told me. What's
strange here, though, is that this polynia is "deep in the ice
pack," he said, and must have formed through other processes
that aren't understood.
"This
is hundreds of kilometres from the ice edge. If we didn't have a
satellite, we wouldn't know it was there." (It measured 80,000
k㎡
at
its peak.)
A
polynia was observed in the same location, in Antarctica's Weddell
Sea, in the 1970s, according to Moore, who's been working with the
Southern Ocean Carbon and Climate Observations and Modelling (SOCCOM)
group, based at Princeton University, to analyze what's going on.
Back then, scientists' observation tools weren't nearly as good, so
that hole remained largely unstudied. Then it went away for four
decades, until last year, when it reopened for a few weeks. Now it's
back again.
"This
is now the second year in a row it's opened after 40 years of not
being there," Moore said. (It opened around September 9.) "We're
still trying to figure out what's going on."
It's
tempting to blame this strange hole on climate change, which is
reshaping so much of the world, including
Antarctica.
But Moore said that's "premature." Scientists can say with
certainty, though, that the polynia will have a wider impact on the
oceans.
"Once
the sea ice melts back, you have this huge temperature contrast
between the ocean and the atmosphere," Moore explained. "It
can start driving convection." Denser, colder water sinks to the
bottom of the ocean, while warmer water comes to the surface, "which
can keep the polynia open once it starts," he said.
Using
observations from satellites and deep sea robots, Moore and his
collaborators are working on as-yet-unpublished research that aims to
answer some of these questions. "Compared to 40 years ago, the
amount of data we have is amazing," he said.
Antarctica
is undergoing massive changes right now, and figuring out why a
gaping hole could suddenly open up will be key to understanding
larger systems at play
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