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Scioglimento dei ghiacci
lo scioglimento dei ghiacci puo' avere serie ripercussioni, compresa la
scarsita' d'acqua in ampie regioni dell'asia.
E' necessario ridurre le emissioni di gas serra a partire da subito
Alessandro Gimona
---------------------------------------------------------
NEWS FROM THE WORLDWATCH INSTITUTE
From the Office of the Chairman
Worldwatch Issue Alert
Alert 2000 - 7
Embargoed for Release
August 29, 2000
6 PM
CLIMATE CHANGE HAS WORLD SKATING ON THIN ICE
Lester R. Brown
If any explorers had been hiking to the North Pole this summer,
they would
have had to swim the last few miles. The discovery of open water at
the Pole by
an ice-breaker cruise ship in mid August surprised many in the
scientific
community.
This finding, combined with two recent studies, provides not only
more
evidence that the Earth's ice cover is melting, but that it is melting
at an
accelerating rate. A study by two Norwegian scientists projects that
within 50
years, the Arctic Ocean could be ice-free during the summer. The
other, a study
by a team of four U.S. scientists, reports that the vast Greenland ice
sheet is
melting.
The projection that the Arctic Ocean will lose all its summer ice
is not
surprising, since an earlier study reported that the thickness of the
ice sheet
has been reduced by 42 percent over the last four decades. The area of
the ice
sheet has also shrunk by 6 percent. Together this thinning and
shrinkage have
reduced the Arctic Ocean ice mass by nearly half.
Meanwhile, Greenland is gaining some ice in the higher altitudes,
but it is
losing much more at lower elevations, particularly along its southern
and
eastern coasts. The huge island of 2.2 million square kilometers
(three times
the size of Texas) is experiencing a net loss of some 51 billion cubic
meters of
water each year, an amount equal to the annual flow of the Nile River.
The Antarctic is also losing ice. In contrast to the North Pole,
which is
covered by the Arctic Sea, the South Pole is covered by the Antarctic
continent,
a land mass roughly the size of the United States. Its continent-sized
ice
sheet, which is on average 2.3 kilometers (1.5 miles) thick, is
relatively
stable. But the ice shelves, the portions of the ice sheet that extend
into the
surrounding seas, are fast disappearing.
A team of U.S. and British scientists reported in 1999 that the
ice shelves
on either side of the Antarctic Peninsula are in full retreat. From
roughly
mid-century through 1997, these areas lost 7,000 square kilometers as
the ice
sheet disintegrated. But then within scarcely a year they lost another
3,000
square kilometers. Delaware-sized icebergs that have broken off are
threatening
ships in the area. The scientists attribute the accelerated ice
melting to a
regional temperature rise of some 2.5 degrees Celsius (4.5 degrees
Fahrenheit)
since 1940.
These are not the only examples of melting. My colleague, Lisa
Mastny, who
has reviewed some 30 studies on this topic, reports that ice is
melting almost
everywhere--and at an accelerating rate. (See Worldwatch News Brief,
March 6,
2000 http://www.worldwatch.org/alerts/000306.html ) The snow/ice mass
is
shrinking in the world's major mountain ranges: the Rocky Mountains,
the Andes,
the Alps, and the Himalayas. In Glacier National Park in Montana, the
number of
glaciers has dwindled from 150 in 1850 to fewer than 50 today. The
U.S.
Geological Survey projects that the remaining glaciers will disappear
within 30
years.
Scientists studying the Quelccaya glacier in the Peruvian Andes
report that
its retreat has accelerated from 3 meters a year between roughly 1970
and 1990
to 30 meters a year since 1990. In Europe's Alps, the shrinkage of the
glacial
area by 35-40 percent since 1850 is expected to continue. These
ancient glaciers
could largely disappear over the next half-century.
Shrinkage of ice masses in the Himalayas has accelerated
alarmingly. In
eastern India, the Dokriani Bamak glacier, which retreated by 16
meters between
1992 and 1997, drew back by a further 20 meters in 1998 alone.
This melting and shrinkage of snow/ice masses should not come as a
total
surprise. Swedish scientist Svente Arrhenius warned at the beginning
of the last
century that burning fossil fuels could raise atmospheric levels of
carbon
dioxide (CO2), creating a greenhouse effect. Atmospheric CO2 levels,
estimated
at 280 parts per million (ppm) before the Industrial Revolution, have
climbed
from 317 ppm in 1960 to 368 ppm in 1999--a gain of 16 percent in only
four
decades.
As CO2 concentrations have risen, so too has Earth's temperature.
Between
1975 and 1999, the average temperature increased from 13.94 degrees
Celsius to
14.35 degrees, a gain of 0.41 degrees or 0.74 degrees Fahrenheit in 24
years.
The warmest 23 years since recordkeeping began in 1866 have all
occurred since
1975.
Researchers are discovering that a modest rise in temperature of
only 1 or 2
degrees Celsius in mountainous regions can dramatically increase the
share of
precipitation falling as rain while decreasing the share coming down
as snow.
The result is more flooding during the rainy season, a shrinking
snow/ice mass,
and less snowmelt to feed rivers during the dry season.
These "reservoirs in the sky," where nature stores fresh water for
use in
the summer as the snow melts, are shrinking and some could disappear
entirely.
This will affect the water supply for cities and for irrigation in
areas
dependent on snowmelt to feed rivers.
If the massive snow/ice mass in the Himalayas--which is the third
largest in
the world, after the Greenlandic and Antarctic ice sheets--continues
to melt, it
will affect the water supply of much of Asia. All of the region's
major
rivers--the Indus, Ganges, Mekong, Yangtze, and Yellow--originate in
the
Himalayas. The melting in the Himalayas could alter the hydrology of
several
Asian countries, including Pakistan, India, Bangladesh, Thailand, Viet
Nam, and
China. Less snowmelt in the summer dry season to feed rivers could
exacerbate
the hydrological poverty already affecting so many in the region. (See
Issue
Alerts 1 and 4 www.worldwatch.org/alerts/indexia.html )
As the ice on land melts and flows to the sea, sea level rises.
Over the
last century, sea level rose by 20-30 centimeters (8-12 inches).
During this
century, the existing climate models indicate it could rise by as much
as 1
meter. If the Greenland ice sheet, which is up to 3.2 kilometers thick
in
places, were to melt entirely, sea level would rise by 7 meters (23
feet).
Even a much more modest rise would affect the low-lying river
floodplains of
Asia, where much of the region's rice is produced. According to a
World Bank
analysis, a 1-meter rise in sea level would cost low-lying Bangladesh
half its
riceland. Numerous low-lying island countries would have to be
evacuated. The
residents of densely populated river valleys of Asia would be forced
inland into
already crowded interiors. Rising sea level could create climate
refugees by the
million in countries such as China, India, Bangladesh, Indonesia, Viet
Nam, and
the Philippines.
Even more disturbing, ice melting itself can accelerate
temperature rise. As
snow/ice masses shrink, less sunlight is reflected back into space.
With more
sunlight absorbed by less reflective surfaces, temperature rises even
faster and
melting accelerates.
We don't have to sit idly by as this scenario unfolds. There may
still be
time to stabilize atmospheric CO2 levels before continuing carbon
emissions
cause climate change to spiral out of control. We have more than
enough wind,
solar, and geothermal energy that can be economically harnessed to
power the
world economy. If we were to incorporate the cost of climate
disruption in the
price of fossil fuels in the form of a carbon tax, investment would
quickly
shift from fossil fuels to these climate-benign energy sources.
The leading automobile companies are all working on fuel cell
engines.
Daimler Chrysler plans to start marketing such an automobile in 2003.
The fuel
of choice for these engines is hydrogen. Even leaders within the oil
industry
recognize that we will eventually shift from a carbon-based energy
economy to a
hydrogen-based one. The question is whether we can make that shift
before
Earth's climate system is irrevocably altered.
- end -
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