This
article was written in 2012, after the lowest ice minimum recorded
last summer
Arctic
Tipping Point:
A
North Pole Without Ice
Scientists
say this year’s record declines in Arctic sea ice extent and volume
are powerful evidence that the giant cap of ice at the top of the
planet is on a trajectory to largely disappear in summer within a
decade or two, with profound global consequences.
by
Fen Montaigne
On
August 26, 2012 Arctic sea ice reached a new record-low summer
extent.
30
August, 2012
As
the northern summer draws to a close, two milestones have been
reached in the Arctic Ocean — record-low sea ice extent, and an
even more dramatic new low in Arctic sea ice volume. This extreme
melting offers dramatic evidence, many scientists say, that the
region’s sea ice has passed a tipping point and that sometime in
the next decade or two the North Pole will be largely ice-free in
summer.
NASA
and U.S. ice experts announced earlier this week that the extent of
Arctic sea ice has dropped to 4.1 million square kilometers (1.58
million square miles) — breaking the previous record set in 2007 —
and will likely continue to fall even farther until mid-September. As
the summer melt season ends, the Arctic Ocean will be covered with 45
percent less ice than the average from 1979 to 2000.
Even
more striking is the precipitous decline in the volume of ice in the
Arctic Ocean. An analysis conducted by the University of Washington’s
Pan Arctic Ice Ocean Model Assimilation System (PIOMAS) estimates
that sea ice volumes fell in late August to roughly 3,500 cubic
kilometers — a 72-percent drop from the 1979-2010 mean.
Peter
Wadhams, who heads the Polar Ocean Physics Group at the University of
Cambridge and who has been measuring Arctic Ocean ice thickness from
British Navy submarines, says that earlier calculations about Arctic
sea ice loss have grossly underestimated how rapidly the ice is
disappearing. He believes that the Arctic is likely to become
ice-free before 2020 and possibly as early as 2015 or 2016 —
decades ahead of projections made just a few years ago.
Mark
Drinkwater, mission scientist for the European Space Agency’s
CryoSat satellite and the agency’s senior advisor on polar regions,
said he and his colleagues have been taken aback by the swiftness of
Arctic sea ice retreat in the last 5 years. “If this rate of
melting [in 2012] is sustained in 2013, we are staring down the
barrel and looking at a summer Arctic which is potentially free of
sea ice within this decade,” Drinkwater said in an e-mail
interview.
A
small number of climate scientists say that natural variability may
be playing a significant role in the rapid retreat of Arctic sea ice,
intensifying human-caused climate change, and they caution against
predicting the imminent demise of the region’s summer sea ice. But
an Extraordinarily low ice levels indicate the summer sea ice has
passed a point of no return. overwhelming majority of Arctic ice
experts say that recent data offer powerful evidence that summer sea
ice has passed a point of no return.
The
dramatic ice loss is being driven by a several key factors,
scientists say. Chief among them is that decades of warming have so
extensively melted and thinned Arctic sea ice that rapidly expanding
areas of dark, open water are absorbing ever-greater amounts of the
sun’s radiation, further warming the region in a vicious cycle.
Second,
swiftly warming air and ocean temperatures in the Arctic have, for
now at least, altered atmospheric activity, with two consequences:
Warmer air is being pulled into the Arctic, and increased storms and
cyclones in summer are not only driving ice out of the Arctic basin,
but also breaking up the ice pack and further exposing more dark
water.
And
finally there is the inescapable reality that steadily rising levels
of carbon dioxide being pumped into the atmosphere by human activity
are continuing to warm the Arctic and the rest of the globe, further
hastening the loss of Arctic Ocean ice. Several experts say that the
only thing that could slow this disappearance — and then only for a
few years — would be a major volcanic eruption that reduces the
amount of the sun’s energy striking the earth.
“It’s
sobering to see the Arctic change so rapidly,” said Ted Scambos,
senior research scientist at the National Snow & Ice Data Center
in Colorado. “Simply staring at the satellite data that we’re
seeing every day is awesome, but in a sad sort of way. It doesn’t
look like the Arctic anymore. The summer ice used to look like a cap
that nearly filled the Arctic basin. It now looks like a raft with
room on every side. You can imagine what it’s going to ‘The
summer ice used to look like a cap…. It now looks like a raft with
room on every side.’ look like when the North Pole is open water,
when there is only a tiny amount of ice left in August and September.
The planet will look a lot different.”
The
loss of the great white dome of ice at the top of the world in summer
will have profound effects, scientists say. These include a reduction
of the amount of solar radiation reflected back into space by the
ice, significant changes to the jet stream and Northern Hemispheric
weather patterns, and even-more rapid warming in the far north,
speeding the melting of Greenland’s massive ice sheets and
increasing global sea levels.
In
addition to these impacts, said Drinkwater, “Increased storminess
will generate ocean wave systems which, un-damped by the presence of
sea ice, will pound the circumpolar north coastlines. Current rates
of coastal permafrost degradation will be accelerated, leading to
significant coastal erosion and reconfiguration of the high-latitude
shoreline. Meanwhile, we have also recently heard about the potential
for release of sub-sea methane deposits and thereby an acceleration
of the current greenhouse effect.”
The
record low sea ice extent in 2007 of 4.2 million square kilometers
was due to some unusual circumstances, including a sunny summer in
the Arctic and higher temperatures. Summer sea ice extent rebounded
somewhat in the next several years, rising to 5.3 million square
kilometers in 2009, giving some hope to mainstream scientists that
Arctic sea ice was not in a “death spiral.”
But
Scambos and other experts say that recent data on plummeting ice
extent and volume show that the Arctic has entered a “new normal”
in which ice decline seems irreversible. Because of thinning ice and
swiftly expanding areas of open water, the Arctic Ocean will no
longer be kept frigid in summer by the reflectivity of snow and ice —
the so-called ice-albedo effect, in which ice and snow reflect a high
percentage of the sun’s energy back into space.
Thick
sea ice that formed over many years is increasingly rare in the
Arctic. In the 1960s, submarines routinely encountered 12-foot-thick
ice around the North Pole and 20-foot-thick ice in some other areas;
now those regions often contain ice that is only three to four feet
thick. Many parts of the Arctic Ocean are now covered with thin,
year-old ice that melts quickly in spring and summer.
This
spring, noted Scambos, extensive late winter snow cover on land
melted unusually rapidly, reaching record low levels by June. Sea ice
across much of the Arctic began to melt 10 to 14 days earlier than in
the preceding few decades. Relatively clear skies from late May
through June further hastened the melting of sea ice, but even as
cloudier weather prevailed in July and August, the record sea ice
retreat continued.
“The
sensitivity of the Arctic to a warm summer is much higher now than it
was in the 1990s or early 2000s,” said Scambos. “What we’re
seeing last year and this year is that 2007 wasn’t a fluke. As
we’ve gone forward a few years, we’re seeing that many different
patterns of weather lead to significant sea ice loss in the Arctic.”
Scambos
does not foresee summer sea ice in the Arctic largely disappearing
this decade, estimating that such an event could occur around 2030,
“plus or minus a decade.” He said the “endgame” of Arctic
summer sea ice will probably mean that around 1 million square
kilometers — about 15 percent of what existed in the mid-20th
century — will remain in the Canadian High Arctic and some other
regions, leaving the North Pole generally ice-free in August and
September.
Drinkwater
said that changing weather patterns, related to more heat and
moisture being released into the Arctic atmosphere, have played a
significant role in accelerating sea ice loss. Sea ice retreat in the
past decade has been accompanied by a trend toward lower atmospheric
pressure and more storms and cyclonic activity, which in turn breaks
up Changing weather patterns have played a significant role in
accelerating sea ice loss. the pack ice and exposes more open water.
A powerful Arctic storm earlier this month did just that, Drinkwater
noted.
He
said that Arctic sea ice could conceivably rebound for some period of
time if atmospheric circulation changes and a pattern known as the
Arctic Oscillation — currently in a positive phase — moves into a
negative phase and ushers in a period of prolonged high atmospheric
pressure and fewer storms. This, said Drinkwater, would enable sea
ice to remain trapped in the Arctic basin and thicken.
“However,”
added Drinkwater, “this seems like blind hope in a system whose
feedbacks all appear geared to getting rid of sea ice.”
Judith
Curry, a climatologist and chair of the School of Earth and
Atmospheric Sciences at the Georgia Institute of Technology, said
that while global warming is “almost certainly” affecting Arctic
sea ice, she cautioned that there is a great deal of annual and
decadal variability in sea ice cover. She said that the next 5 to 10
years could see a shift in Arctic sea ice behavior, though exactly in
which direction is difficult to predict.
“I
don’t see [the] summer of 2012 portending some sort of near-term
`spiral of death’ in the sea ice behavior,” Curry said in an
e-mail interview. “I don’t think this apparent record sea ice
minimum is of particular significance in our understanding of climate
variability and change of Arctic sea ice.”
The
loss of Arctic summer sea ice and the rapid warming of the Far North
are altering the jet stream over North America, Europe, and Russia.
As Jennifer Francis writes, scientists are now just beginning to
understand how these profound shifts may be increasing the likelihood
of more persistent and extreme weather.
Jay Zwally, chief cryospheric scientist at NASA’s Goddard
Space Flight Center and an observer of Arctic ice for 40 years,
places little stock in the likelihood of a reversal of disappearing
Arctic ice. New satellite technology has given scientists the ability
to measure the height of sea ice above the water, and hence ice
volume. Those measurements, he said, have vividly underscored that
Arctic sea ice is in a swoon.
For
example, a recent analysis of data from CryoSat and NASA’s ICESat
satellite estimates that the volume of sea ice in a large area of the
central Arctic Ocean has plummeted in late winter — February and
March — by nearly half in just eight years, from an estimated
13,000 cubic kilometers in 2004 to 7,000 cubic kilometers in 2012.
“We’ve
gone through a tipping point, and of all the things a tipping point
applies to, sea ice is the most appropriate, because the idea is when
it goes below a certain thickness it doesn’t go back under present
conditions,” said Zwally. “People can get hung up on the
specifics and lose track of the big picture, which is that it’s
getting worse and it’s going to get [even] worse.”
Fen
Montaigne is senior editor of Yale Environment 360 and author of
the book Fraser’s Penguins: A Journey to the Future in Antarctica.
His work has appeared in The New Yorker, National Geographic,
Outside, Smithsonian, and other magazines. He has written previously
for Yale Environment 360 about the consequences of a warming
Antarctica and about how receding sea ice will affect the polar
marine food chain.
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