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By Andrew C. Revkin
The New York Times
Tuesday 02 October 2007
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Retreat.
A photograph taken in August from an icebreaker research cruise in the
Arctic Ocean, about 600 miles north of the Alaska coastline.
(Photo: Andy Armstrong / NOAA)
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The
Arctic ice cap shrank so much this summer that waves briefly lapped
along two long-imagined Arctic shipping routes, the Northwest Passage
over Canada and the Northern Sea Route over Russia.
Overall, the floating ice dwindled to an extent unparalleled in a century or more, by several estimates.
Now
the six-month dark season has returned to the North Pole. In the
deepening chill, new ice is already spreading over vast stretches of
the Arctic Ocean. Astonished by the summer's changes, scientists are
studying the forces that exposed one million square miles of open water
- six Californias - beyond the average since satellites started
measurements in 1979.
At
a recent gathering of sea-ice experts at the University of Alaska in
Fairbanks, Hajo Eicken, a geophysicist, summarized it this way: "Our
stock in trade seems to be going away."
Scientists are also unnerved by the summer's implications for the future, and their ability to predict it.
Complicating
the picture, the striking Arctic change was as much a result of ice
moving as melting, many say. A new study, led by Son Nghiem at NASA's
Jet Propulsion Laboratory and appearing this week in Geophysical
Research Letters, used satellites and buoys to show that winds since
2000 had pushed huge amounts of thick old ice out of the Arctic basin
past Greenland. The thin floes that formed on the resulting open water
melted quicker or could be shuffled together by winds and similarly
expelled, the authors said.
The
pace of change has far exceeded what had been estimated by almost all
the simulations used to envision how the Arctic will respond to rising
concentrations of greenhouse gases linked to global warming. But that
disconnect can cut two ways. Are the models overly conservative? Or are
they missing natural influences that can cause wide swings in ice and
temperature, thereby dwarfing the slow background warming?
The world is paying more attention than ever.
Russia,
Canada and Denmark, prompted in part by years of warming and the ice
retreat this year, ratcheted up rhetoric and actions aimed at securing
sea routes and seabed resources.
Proponents
of cuts in greenhouse gases cited the meltdown as proof that human
activities are propelling a slide toward climate calamity.
Arctic
experts say things are not that simple. More than a dozen experts said
in interviews that the extreme summer ice retreat had revealed at least
as much about what remains unknown in the Arctic as what is clear.
Still, many of those scientists said they were becoming convinced that
the system is heading toward a new, more watery state, and that
human-caused global warming is playing a significant role.
For
one thing, experts are having trouble finding any records from Russia,
Alaska or elsewhere pointing to such a widespread Arctic ice retreat in
recent times, adding credence to the idea that humans may have tipped
the balance. Many scientists say the last substantial warming in the
region, peaking in the 1930s, mainly affected areas near Greenland and
Scandinavia.
Some
scientists who have long doubted that a human influence could be
clearly discerned in the Arctic's changing climate now agree that the
trend is hard to ascribe to anything else.
"We
used to argue that a lot of the variability up to the late 1990s was
induced by changes in the winds, natural changes not obviously related
to global warming," said John Michael Wallace, a scientist at the
University of Washington. "But changes in the last few years make you
have to question that. I'm much more open to the idea that we might
have passed a point where it's becoming essentially irreversible."
Experts
say the ice retreat is likely to be even bigger next summer because
this winter's freeze is starting from such a huge ice deficit. At least
one researcher, Wieslaw Maslowski of the Naval Postgraduate School in
Monterey, Calif., projects a blue Arctic Ocean in summers by 2013.
In
essence, Arctic waters may be behaving more like those around
Antarctica, where a broad fringe of sea ice builds each austral winter
and nearly disappears in the summer. (Reflecting the different
geography and dynamics at the two poles, there has been a slight
increase in sea-ice area around Antarctica in recent decades.)
While
open Arctic waters could be a boon for shipping, fishing and oil
exploration, an annual seesawing between ice and no ice could be a
particularly harsh jolt to polar bears.
Many
Arctic researchers warned that it was still far too soon to start
sending container ships over the top of the world. "Natural variations
could turn around and counteract the greenhouse-gas-forced change,
perhaps stabilizing the ice for a bit," said Marika Holland, of the
National Center for Atmospheric Research in Boulder, Colo.
But,
she added, that will not last. "Eventually the natural variations would
again reinforce the human-driven change, perhaps leading to even more
rapid retreat," Dr. Holland said. "So I wouldn't sign any shipping
contracts for the next 5 to 10 years, but maybe the next 20 to 30."
While
experts debate details, many agree that the vanishing act of the sea
ice this year was probably caused by superimposed forces including
heat-trapping clouds and water vapor in the air, as well as the
ocean-heating influence of unusually sunny skies in June and July.
Other important factors were warm winds flowing from Siberia around a
high-pressure system parked over the ocean. The winds not only would
have melted thin ice but also pushed floes offshore where currents and
winds could push them out of the Arctic Ocean.
But
another factor was probably involved, one with roots going back to
about 1989. At that time, a periodic flip in winds and pressure
patterns over the Arctic Ocean, called the Arctic Oscillation, settled
into a phase that tended to stop ice from drifting in a gyre for years,
so it could thicken, and instead carried it out to the North Atlantic.
The
new NASA study of expelled old ice builds on previous measurements
showing that the proportion of thick, durable floes that were at least
10 years old dropped to 2 percent this spring from 80 percent in the
spring of 1987, said Ignatius G. Rigor, an ice expert at the University
of Washington and an author of the new NASA-led study.
Without
the thick ice, which can endure months of nonstop summer sunshine, more
dark open water and thin ice absorbed solar energy, adding to melting
and delaying the winter freeze.
The
thinner fresh-formed ice was also more vulnerable to melting from heat
held near the ocean surface by clouds and water vapor. This may be
where the rising influence of humans on the global climate system could
be exerting the biggest regional influence, said Jennifer A. Francis of
Rutgers University.
Other
Arctic experts, including Dr. Maslowski in Monterey and Igor V.
Polyakov at the University of Alaska, Fairbanks, also see a role in
rising flows of warm water entering the Arctic Ocean through the Bering
Strait between Alaska and Russia, and in deep currents running north
from the Atlantic Ocean near Scandinavia.
A
host of Arctic scientists say it is too soon to know if the global
greenhouse effect has already tipped the system to a condition in which
sea ice in summers will be routinely limited to a few clotted
passageways in northern Canada.
But
at the university in Fairbanks - where signs of northern warming
include sinkholes from thawing permafrost around its Arctic research
center - Dr. Eicken and other experts are having a hard time conceiving
a situation that could reverse the trends.
"The
Arctic may have another ace up her sleeve to help the ice grow back,"
Dr. Eicken said. "But from all we can tell right now, the means for
that are quite limited."
(In accordance with Title 17 U.S.C. Section 107, this material is distributed without profit to those who have expressed a prior interest in receiving the included information for research and educational purposes. h o t g l o b e has no affiliation whatsoever with the originator of this article nor is h o t g l o b e endorsed or sponsored by the originator.)
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