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Politics : The Donkey's Inn -- Ignore unavailable to you. Want to Upgrade?


To: Mephisto who wrote (7436)9/23/2003 6:42:38 PM
From: Mephisto  Respond to of 15516
 
Arctic's Biggest Ice Shelf, a Sentinel of
Climate Change, Cracks Apart:

The breakup is apparent evidence of global warming.
It also has drained a freshwater lake
containing a rare ecosystem.


By Usha Lee McFarling, Times Staff Writer

The largest ice shelf in the Arctic - an 80-foot-thick
slab of ice nearly the size of Lake Tahoe - has broken
up, providing more evidence that the Earth's polar
regions are responding to ongoing and accelerating
rates of climatic change, researchers reported Monday.

The Ward Hunt ice shelf, located 500 miles from the
North Pole on the edge of Canada's Ellesmere Island,
has broken into two main parts and a series of ice
islands. A massive freshwater lake long held back by
the ice has drained away.

"Large blocks of ice are moving out. It's really a
breakup," said Warwick Vincent, a professor of
biology at Laval University in Quebec and co-author of
the report, which will be published in an upcoming issue
of the journal Geophysical Review Letters. "We'd been
measuring incremental changes each year. Suddenly in
one year, everything changed."

While far larger shelves of ice have cracked off the
edges of Antarctica, this is the largest ice separation in
the Arctic, occurring in an area of the eastern Arctic
long thought to be more protected against the gradual
warming of the planet.

"This type of catastrophic [event] is quite
unprecedented," said Martin Jeffries, a professor of
geophysics at the University of Alaska Fairbanks and
co-author of the report.

Because of their longevity and sensitivity to
temperature, ice shelves are considered "sentinels of
climate change." In recent years, scientists have seen ice
shelves the size of Rhode Island break off of western
Antarctica as it warms and have measured glaciers'
retreat in response to warmer temperatures throughout
the western Arctic.

Weather data recorded at the nearby military station
Alert on Ellesmere Island show that temperatures there
have been warming since 1967 at the same rate as in
western Antarctica: about one degree Fahrenheit per
decade. The average July temperature of recent years
of 34 degrees was above the temperature - 32
degrees - at which ice shelves are known to break up.

The researchers said they considered the weakening of
the ice additional evidence of climate change in the high
Arctic and said the report fit with studies that show
global warming trends are connected to the human
production of greenhouse gases. Those trends have been seen first and amplified
in the Arctic.

But they said other factors, including ocean circulation and atmospheric patterns
that can last for decades, could be contributing to the changes in the ice.

"The picture is a little murky," Jeffries said.

Jeffries, who has worked on the region's ice sheets for two decades, said the ice
appears to have thinned dramatically in that time. The Ward Hunt ice shelf was
measured at 150 feet thick in 1980 and now appears to be less than half that in
some places.

The ice shelf has lost 90% of its area since 1907, when explorer Robert E. Peary
crossed it on his way to the North Pole and complained bitterly about its
undulating terrain.

Researchers were lucky to catch the breakup in such a remote and relatively
unstudied area. Derek Mueller, a graduate student of Vincent's, had reached the
ice shelf by helicopter last summer to study the strange microbes living there when
he saw that the massive cracks extended all the way through the ice.

Using a satellite phone, he called Vincent. Canada's RADARSAT satellite then
captured fresh images of the ice shelf as it was breaking up.

Vincent is very concerned about the ecosystem he and his students were
studying. It has basically been flushed out to sea. The weakening and cracking of
the ice shelf allowed a freshwater lake that had been dammed behind the ice to
drain suddenly.

The ice shelf kept about 140 feet of freshwater pooled atop 1,200 feet of denser
seawater. The layers of fresh and salty water supported an ecosystem of strange
microbes, or extremophiles, that are of particular interest to scientists trying to
understand the limits of life on Earth and in outer space.

"The whole lake just drained. It just disappeared entirely," Vincent said. "We're at
a point where we're starting to lose these unique cryo-ecosystems of the north
before we can understand them."

Other researchers are concerned about the increasing amount of fresh water
pouring into the Arctic Ocean from breaking ice shelves, melting glaciers and
rain-swollen rivers.

Cold, salty water in the Arctic and North Atlantic oceans plays a major role in
driving ocean currents that transport heat around the globe.

One of the most important of these is the Gulf Stream, which carries warm water
up the East Coast of the United States and across the Atlantic to northern
Europe.

In previous geological eras, warmer climates and the release of freshwater lakes
that had been dammed by ice have caused this current to slow and shut down,
drastically cooling parts of Europe.

A study in the journal Science in December reported massive amounts of fresh
water entering the Arctic from Russia's largest rivers, due to increases in
precipitation linked to warmer temperatures.

If temperatures rise globally by several degrees in the next century, as many
scientists predict, increased river runoff, melting of glaciers on Greenland and
melting of ice shelves "would bring us well within the range of what models say
could be a serious disruption to ocean circulation," said Bruce Peterson, a senior
scientist at the Marine Biological Laboratory in Woods Hole, Mass.

While the amount of fresh water released from the breaking of the Ward Hunt ice
shelf is relatively small, some scientists say it is part of a larger pattern of
freshening of ocean waters that could prove dangerous in the future.

"The question is, at what point do those currents become unhappy?" said Richard
Alley, a professor of geosciences at Penn State University and an expert on ice
sheets and abrupt climate change. "We're just not good enough to tell right now."

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