-Caveat Lector-

Thaw in Greenland threatens new ice age
http://www.guardian.co.uk/climatechange/story/0,12374,872609,00.html
This week's big chill could prove a taster of winters to come

Paul Brown, environment correspondent
Saturday January 11, 2003
The Guardian

The snowfalls of the past week may be just a taster of what is to come, if the latest
predictions from scientists are correct. The amount of ice melting from the surface of 
the
Greenland ice sheet broke all known records last year, threatening a rapid rise in sea
levels and a return of very cold winters to Britain because of a slowing down in the 
Gulf
Stream.

Already the Gulf Stream, which bathes the west coast of Britain in warm water from the
Gulf of Mexico and keeps the country much milder than normal for such northern
latitudes, is slowing down. Even greater melting of the Greenland ice could shut off 
the
currents altogether, allowing depressions to dump snow rather than instead of rain in
Britain and leading to a much colder continental climate, as has been experienced in
the past week.

As happens on the eastern seaboard of Canada, which on the same latitude, the sea
could freeze and snow lie for weeks or months instead of a day of two.

Last year large areas of the Greenland ice shelf, previously too high and too cold to
melt, began pouring billions of gallons of fresh water into the northern Atlantic. 
Melted
water trapped between the ice and the rock beneath is causing an acceleration of
glaciers breaking off in huge chunks and increasing the number of icebergs.

According to scientists at the University of Colorado a very dramatic melting trend has
been in progress since 1979. Extreme melt years were 1991, 1995 and 2002.

The Greenland ice sheet's maximum melt area increased on average by 16% from
1979 to 2002. This year's maximum melt extent of 264,400 square miles exceeds by
2.6 times the melt area measured in 1992. In particular, the northern and north-eastern
part of the ice sheet experienced melting reaching up to an elevation of 2,000 metres
(6,560ft).

This is the first time this area of the giant island, closest to the north pole, has 
suffered
this kind of melting. The Colorado-based Cooperative Institute for Research in
Environmental Sciences also found that temperatures during the summer of 2002 were
unusually warm over much of the Arctic ocean.

"Since the season also was characterised by very stormy conditions, we believe these
two factors contributed to extensive melt and break-up of the icepack," said research
associate Mark Serreze, the lead author of the study, which was presented at a meeting
of the American Geophysical Union.

Sea ice in the Arctic last year was at the lowest since satellite measurements began.

Mr Serreze said accelerated melting of sea ice, along with runoff from the Greenland 
ice
sheet, was bad news for British weather moderated by the Gulf Stream. The warm water
from the tropics now travels north past British shores and warms the western coastlines
of Europe as far north as Norway before sinking to the bottom of the ocean and
returning south.

This deep water convection in the north Atlantic has already been noted to be slowing
down by British scientists, and US scientists say the trend could profoundly impact
global ocean circulation and climate. "In other studies, changes in the north Atlantic
circulation have been implicated in starting and stopping northern hemisphere ice
ages," Mr Serreze said.

Climatologist Konrad Steffen, a professor of geography at Colorado, said a change in
the Greenland climate towards warmer conditions would lead to an increase in the rate
of sea level rise, mainly due to the dynamic response of the large ice sheet rather 
than
just the surface melting.

"For every degree increase in the mean annual temperature near Greenland, the rate of
sea level rise increases by about 10%," Professor Steffen said. Oceans are now rising
by a little more than half an inch every 10 years.

Both sea ice and glacier ice cool the earth, reflecting back into space about 80% of
springtime sunshine and 40% -50% during the summer melt. But winter sea ice cover
slows heat loss from the relatively warm ocean to the cold atmosphere. Without large
sea ice masses at the poles to moderate the energy balance, warming escalates.

Guardian Unlimited © Guardian Newspapers Limited 2003
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