Climate Tipping Points: In From the Cold

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“If a very small warming makes such a difference,”
Alley said, “it raises the question of what happens
when more warming occurs.”
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SCIENCE
VOL 319 11 JANUARY 2008

CLIMATE TIPPING POINTS COME IN FROM THE COLD

Tipping points, once considered too alarmist for proper scientific
circles, have entered the climate change mainstream.

At the meeting, a nearly packed half-day session considered the
prospects for a climate system that is still creeping through change
but might soon cross a threshold into an entirely new way of
operating. The new climate regime may have no sea ice in Arctic
summers, a much smaller ice sheet on West Antarctica and higher sea
levels, or wildly redirected storm tracks. Current understanding of
climate allows that such drastic transitions can happen, the speakers
agreed. Earth may even be in the midst of one now.

As evidence, glaciologist Richard Alley of Pennsylvania State
University in State College cited Earth’s response to the warming
that has occurred over the past 3 decades. Compared with the soaring
global temperatures that the strengthening greenhouse could drive
through the rest of this century, that warming has been rather small,
Alley said. Yet it is having immediate and often unexpected effects,
he observed. Since the 1960s, mountain glaciers around the world have
begun to shrink and are dwindling rapidly. Arctic summer sea ice took
a severe hit last year after decades of slow losses. And the
Greenland ice sheet is now clearly shrinking under some unexpected
attacks. Warming seas are weakening glaciers’ surprisingly fragile
ice tongues, which help slow glaciers’ rush to the sea. And meltwater
on the surfaces of glaciers is plunging down giant cracks to glacier
beds, where it’s lubricating the glaciers’ seaward slip-sliding. ”

If a very small warming makes such a difference,” Alley said, “it
raises the question of what happens when more warming occurs.” Sea
ice specialist Josefino Comiso of NASA’s Goddard Space Flight Center
in Greenbelt, Maryland, said at the meeting that in the Arctic, “the
tipping point for perennial sea ice has likely already been reached.”
Ice persisting from year to year has not been steadily shrinking in
area, he said. The decline of summer sea ice accelerated in the
mid-1990s; since then, summer ice has been disappearing more than
three times faster than before. And the feedback between solar
warming of newly ice-free Arctic waters and the loss of still more
ice has become more and more obvious.

Only colder summers and colder winters can save summer sea ice from
oblivion, he said, an unlikely development at this point. Other
speakers presented possible tipping points that have gotten less
attention: an eventual sudden shift in jet streams that would bring
rapid climate change to North America and Europe and the abrupt
collapse of the Amazon tropical forest, among others. Clearly, the
possibilities are proliferating faster than researchers can confirm
or deny them.    -R.A.K.

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The meeting discussed above was the December, 2007 annual Fall
Meeting of the American Geophysical Union, an association of
scientific societies including specialists in the atmospheric,
biological, chemical, geologic and other sciences.  L.O.

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Climate Change, Corporate “Development,” and the Maine North Woods

Climate Change, Corporate “Development,” and the Maine North Woods

Many people are not aware that a respectably sized chunk of wild forest
ecosystem struggles for survival in northern Maine. The Maine North Woods
comprise part of the southeastern edge of the Great North Woods, which
stretch in an arc across the North American continent (mostly in Canada)
from the Atlantic Seaboard to the Great Plains. The Maine North Woods
encompass most of the northern half of the state and provide a home for
rare species—including wolves and Canada lynx. It is the largest wild,
undeveloped area east of the Mississippi River.

Seattle-based Plum Creek Real Estate Investment Corporation—the nation’s
largest private landowner—has proposed a massive development for the heart
of the Moosehead Lake region. It is the largest subdivision ever proposed
in Maine. An initial proposal submitted in April 2005 to Maine’s Land Use
Regulation Commission (LURC) was withdrawn after significant public
outcry. A revised proposal was submitted in April 2006 and withdrawn again
after further significant public outcry. The latest proposal was submitted
in April 2007 and amended in August and October 2007. Plum Creek Timber
Co. is one of the nation’s (indeed, the continent’s) largest private
landowners. Many people in the forest defense movement are depressingly
familiar with Plum Creek’s dismal forest management practices (such as in
Wisconsin, Montana, and Washington states), as well as its propensity
toward “developing” forested wildlands into extravagant, exclusive
playgrounds for those humans rich, white, and callous (or clueless) enough
to afford them. Now Plum Creek has set its sights on northern Maine’s
Moosehead Lake Region for another such resort complex. Fortunately for
this priceless ecosystem, Mainers are far from stupid and have been
tracking these plans very carefully for quite some time now.

Continue reading

Future Ocean Conditions Likely to Downsize Marine Life

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“It’s warmer, marine mammals and birds are having massive die-offs,
there are invasive species-in general, it’s changing to a more temperate
ecosystem that’s not going to be as productive.”

“It’s all a good start that people get worried about melting ice and rising
sea levels,” he said. “But we’re now driving a comprehensive change in
the way Earth’s ecosystem works-and some of these changes don’t bode
well for its future.”
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University of Southern California
Public release date: 11-Jan-2008

Greenhouse ocean may downsize fish
By 2100, warmer oceans with more carbon dioxide may no longer sustain
1 of the world’s most productive fisheries, says USC marine ecologist

The last fish you ate probably came from the Bering Sea.

But during this century, the sea’s rich food web-stretching from
Alaska to Russia-could fray as algae adapt to greenhouse conditions.

“All the fish that ends up in McDonald’s, fish sandwiches-that’s all
Bering Sea fish,” said USC marine ecologist Dave Hutchins, whose
former student at the University of Delaware, Clinton Hare, led
research published Dec. 20 in Marine Ecology Progress Series, a
leading journal in the field.

At present, the Bering Sea provides roughly half the fish caught in
U.S. waters each year and nearly a third caught worldwide.

“The experiments we did up there definitely suggest that the changing
ecosystem may support less of what we’re harvesting-things like
pollock and hake,” Hutchins said.

While the study must be interpreted cautiously, its implications are
harrowing, Hutchins said, especially since the Bering Sea is already
warming.

“It’s kind of a canary in a coal mine because it appears to be
showing climate change effects before the rest of the ocean,” he
noted.

“It’s warmer, marine mammals and birds are having massive die-offs,
there are invasive species-in general, it’s changing to a more
temperate ecosystem that’s not going to be as productive.”

Carbon dioxide’s direct effects on the ocean are often overlooked by
the public.

“It’s all a good start that people get worried about melting ice and
rising sea levels,” he said. “But we’re now driving a comprehensive
change in the way Earth’s ecosystem works-and some of these changes
don’t bode well for its future.”

The study examined how climate change affects algal communities of
phytoplankton, the heart of marine food webs.

Phytoplankton use sunlight to convert carbon dioxide into
carbon-based food. As small fish eat the plankton and bigger fish eat
the smaller fish, an entire ecosystem develops.

The Bering Sea is highly productive thanks mainly to diatoms, a large
type of phytoplankton.

“Because they’re large, diatoms are eaten by large zooplankton, which
are then eaten by large fish,” Hutchins explained.

The scientists found that greenhouse conditions favored smaller types
of phytoplankton over diatoms. Such a shift would ripple up the food
chain: as diatoms become scarce, animals that eat diatoms would
become scarce, and so forth.

“The food chain seems to be changing in a way that is not supporting
these top predators, of which, of course, we’re the biggest,”
Hutchins said.

A shift away from diatoms towards smaller phytoplankton could also
undermine a key climate regulator called the “biological pump.”

When diatoms die, their heavier carbon-based remains sink to the
seafloor. This creates a “pump” whereby diatoms transport carbon from
the atmosphere into deep-sea storage, where it remains for at least
1,000 years.

“While smaller species often fix more carbon, they end up
re-releasing CO2 in the surface ocean rather than storing it for long
periods as the diatom-based community can do,” Hutchins explained.

This scenario could make the ocean less able to soak up atmospheric
carbon dioxide.

“Right now, the ocean biology is sort of on our side,” Hutchins said.
“About 50 percent of fossil fuel emissions since the industrial
revolution is in the ocean, so if we didn’t have the ocean,
atmospheric CO2 would be roughly twice what it is now.”

Hutchins and colleagues are doing related experiments in the north
Atlantic Ocean and the Ross Sea, near Antarctica. The basic dynamics
of a greenhouse ocean are not well understood, he noted.

“We’re trying to make a contribution by doing predictive experimental
research that will help us understand where we’re headed,” he said.
“It’s unprecedented the rate at which things are shifting around.”

The researchers collected the algae samples from the Bering Sea’s
central basin and the southeastern continental shelf. They incubated
the phytoplankton onboard, simulating sea surface temperatures and
carbon dioxide concentrations predicted for 2100.

Each of these variables was tested together and independently. Ratios
of diatom to nanophytoplankton in manipulated samples were then
compared with those in plankton grown under present conditions.

The scientists found that photosynthesis in greenhouse samples sped
up two to three times current rates. However, community composition
shifted from diatoms to the smaller nanophytoplankton.

Temperature was the key driver of the shift with secondary impacts
from the increased carbon dioxide concentrations, according to the
study.

###

Hutchins and Hare’s collaborators were Karine Leblanc of the Centre
National de la Recherche Scientifique, in France; Giacomo DiTullio,
Peter Lee and Sarah Riseman of the College of Charleston; Raphael
Kudela of the University of California at Santa Cruz; and Yaohong
Zhang of the University of Delaware.

The National Science Foundation supported the research.

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James Hansen: Climate and Wildlife

http://pubs.giss.nasa.gov/abstracts/inpress/Hansen_1.html

ABSTRACT
Hansen 2008, in press   Complete document is not available.

Hansen, J., 2008: Tipping point: Perspective of a climatologist. In
The State of the Wild 2008: A Global Portrait of Wildlife, Wildlands,
and Oceans. E. Fearn and K.H. Redford, Eds. Wildlife Conservation
Society/Island Press, in press.

I describe how two fundamental properties of our climate system, its
predominance of “positive feedbacks” and its ponderous inertia, have
together brought climate to a great tipping point, a planetary
emergency. I then discuss emerging impacts of climate change on the
wild. Finally I summarize fundamental data on fossil fuels, the main
driver of climate change, providing an outline of actions needed to
reverse the forces driving climate change.

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With a co-author, Hansen previously published an analysis of whether
peak oil might come soon enough to bring some relief to the pressures
pushing toward dangerous change of climate.
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