|
CLIMATE CHANGE HAS WORLD SKATING ON THIN ICE Lester R.
Brown August 29, 2000
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 -
FOR DATA, GRAPHS, AND ADDITIONAL INFORMATION
www.worldwatch.org/alerts/indexia.html
If you know someone who might like to receive the Issue
Alerts regularly, please contact Reah Janise Kauffman rjkauffman@worldwatch.org
. COPYRIGHT: 2000 Worldwatch Institute CONTACT: Reah Janise Kauffman PHONE:
(202) 452-1992 x 514 FAX: (202) 296-7365 |