Cold facts of global warming
By Nicholas Booth
Copyright 1999 The Times (UK)
March 3, 1999
 In Antarctica, you are either too hot or too cold. That's
how Dr David Sugden 
describes living conditions at the South Pole where he moves around
in the 
coruscating cold 
in layers of clothes and impressive-looking hoods. 
 He could just as well be describing the enduring
controversy about the frozen 
continent's climate. For years, glaciologists have debated whether
the 
Antarctic climate has undergone periodic warmings or remained
freezing cold. As 
the man who discovered the world's oldest ice, Dr Sugden 
believes he has solved the mystery.  
 A professor of geography at Edinburgh University, he
believes he has proof 
that the Antarctic has long been in deep freeze, implying that the
Earth's 
climate as a whole is far more resilient than had been thought.
Reports of 
catastrophic effects to come from 
global warming may well be exaggerated, he says. 
 
"We've argued that the Antarctic 
ice has been very stable for a long time. Now we have shown that
there is a 
genuinely large lump of ancient ice in a dry valley. Its survival
implies that 
the climate must have been similar in the past." 
 Few people thought that ice could survive for eight
million years, even 
in Antarctica. Along with American colleagues, Dr Sugden published
his findings 
in 1995, but there was little reaction from the outside world.
Chris McKay, a 
biologist with Nasa, observes: 
"They produced a paper called 'Miocene Ice in Antarctica'.
That's another way of 
saying 'This is the world's oldest 
ice'. Most ice on Earth has only been around for a few hundred
thousand years." 
 Recently, Mr McKay shared a tent with Dr Sugden on the
floor of Beacon Valley 
in Antarctica, where they were equipped with drills and
ground-penetrating 
radars. 
 The dry valleys are associated with 
tragedies of earlier expeditions. They were discovered by Robert
Falcon Scott 
on his first visit to the southern continent in 1905. Even by the
breathtaking 
standards of vertiginous landscapes of sculpted ice, the valleys
were a 
revelation. Climatically, they are bizarre - drier than the Gobi
desert with 
little water vapour available to 
fall as snow. They are cut off from the nearby ice by the towering 
Transantarctic Mountains and, over the millennia, have been
peppered with 
volcanic ash and dust. 
 
"I've been down to the south a dozen times," Dr Sugden
says. 
"It came as quite a surprise to find old, glacial ice under
the 
rubble of the dry valleys." 
 The ice in Antarctica plays a fundamental role in
modifying climate. Although 
it covers only about 10 per cent of the total landmass on Earth,
Antarctica 
contains about 90 per cent of the world's ice. Polar icecaps 
keep the Earth cool, with the ice limiting the exchange of heat
between the 
atmosphere and the ocean in the polar regions. What happens to
Antarctic ice is 
viewed as a marker for global 
climate change: the first signs of 
global warming are likely be seen at the South Pole. 
 The controversy stems from the disputed 
age of the ice in the dry valleys and hangs on the question of how
hot or cold 
the climate has been in the past. The advocates of periodically
warmer climates 
have examined microscopic flora which could have thrived in warmer
times if the 
surrounding regions were deglaciated. 
"We think these things blew in from elsewhere at a 
later date," Dr Sugden says. 
"They are found so widely in the ice over the rest of the
continent." 
 He and his colleagues have come at the problem from a
different angle: 
volcanic ash. There are active volcanoes in Antarctica today; in
the past, they 
could have spewed untold quantities of ash and dust into the
atmosphere which 
rained down into the dry valleys. By looking at argon isotopes
within the ash, 
Dr Sugden's team has dated the ice to eight million years. After
their earlier 
paper, more recent extensive analyses have bolstered their
findings. 
"When you have nine out of ten grains giving you this age, you
can be 
pretty certain you're right," he says. 
 But could the ice have been just a few metres deep and a
more recent 
phenomenon, caused by water seeping into the moraines when warmed
by sunlight 
during the austral summer? Samples of the ice, analysed by Belgian
researchers, 
show that their structure is 
glacial, having the characteristic shape of snowflakes packed
together over 
time. And the ground radar used on the most recent research trip
shows that the 
ice extends for at least 120 metres below the surface. 
 What does this mean? Dr Sugden believes that it could have
a curious outcome 
on the 
future of the continent. The Antarctic is bisected by the
Transantarctic 
Mountains. Climatically, it is a continent of two halves, a
distinction which 
informs the debate on 
global warming. 
 Western Antarctica is more unstable because most of the
land on which the ice 
rests is below sea level. Ice continues to spread 
out to the sea, forming ice shelves that are glued to the landmass
by the 
freezing cold. 
"The ice is like a ship that is aground," Dr Sugden says.
"Its weight keeps it moored there." If temperatures rise,
the sea level could rise by a few metres, though this 
has not been measured yet. 
 
But Eastern Antarctica, in which the dry valleys are located, is a
different 
matter. Containing ten times more ice than the western half, the
results from 
Beacon Valley suggest that it is much more stable. Eastern
Antarctica is 
effectively a giant dome of ice that rises some four 
kilometres above sea level because its underlying rock is higher. 
 Dr Sugden believes that this larger part of the ice sheet
will act as its own 
thermostat and control the climatic conditions. Increase the
temperature and 
water will go into the atmosphere as vapour, form snow and,
paradoxically, 
increase the snow cover. 
"To get 
rid of this ice, you're going to have to do something very, very
drastic," he adds. 
"Our findings show that the climate has been stable in the
past and would be 
expected to remain so." 
 If all the ice in Antarctica were melted, then global sea
levels could rise by 
60 metres. But Dr Sugden believes that the curious ice found 
in the dry valleys is telling us that that is a very unlikely event
indeed. 
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