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Deforestation and land
degradation, pollution of marine and fresh waters and depletion of the
ozone layer–these and other environmental issues have received widespread
attention in the media. These problems somehow seem local and solvable.
A landfill site can be monitored by a local authority and just stopping
its use will significantly reduce the risk of pollutants entering the
water supply. If necessary we have the technology to clean it up. Global
warming is thought to be different. It is said to be a global manifestation
of our pollution of the planet. It also grips us with the fear of the
unknown–an insidious global danger. The solutions proposed range
from dramatic changes in lifestyle to de-industrialisation and population
control. Many fear that the action we take now might already be too little
too late.
What
are the facts? There is much anecdotal evidence that global warming is
occurring– hurricanes in the Caribbean, the break-up of Antarctic
ice shelves and warm summers in England. But what are the likely implications
of warming and is the science of climate change now scarcely in dispute
as is widely claimed? Global warming theory became scientific orthodoxy
with the publication of the first report of the Intergovernmental Panel
on Climate Change in 1990. The IPCC was set up in 1988 by the UN Environmental
Programme and the World Meteorological Organization to assess the scientific
evidence on climate change and its impact and to formulate a response.
In its 1992 report the IPCC predicted a best estimate of a global mean
temperature rise of 2.5°C in the next 100 years
and 0.5°C by 2010. Net emissions from changes in tropical land use
have also been brought into the frame as responsible for 15 per cent of
net anthropogenic emissions (Radiative Forcing of Climate Change, Report
of the Scientific Assessment Working Group of the IPCC 1994).
Assuming
this to be the case for the moment, does it matter? The most important
point to appreciate from studies of past climates is that the earths
climate is forever changing. We live in the period of time that geographers
call the Holocene. This is the present warm period that has lasted for
about 10,000 years. Prior to the Holocene was the Pleistocene which is
synonymous with the alternation of ice ages, lasting about 100,000 years
and short inter-glacials, lasting about 10,000 to 20,000 years. In fact
most earth scientists regard the Holocene as an inter-glacial, with the
onset of a new ice age not too far distant in time. The past temperature
(palaeo-climate) record is preserved in the ice sheets of Greenland and
Antarctica. In the last few years much effort has been directed at extracting
continuous ice cores of 3-4 kilometres depth which hold high resolution
palaeo-climate records of the last 100,000 to 250,000 years. These tell
us that compared to the more distant past, we have had remarkably stable
temperatures in the Holocene. Even in the Holocene temperature change
is observed.
Change is the norm and nature has no preferred state. Should we have a
preferred state from a human-centred perspective? Reconstruction of palaeo-climate
and palaeo-environments shows that the ice-age earth was a truly dreadful
place. As well as mean global temperatures more than 4°C colder than
today, ice age climates were more arid, there was no Indian monsoon, vegetation
survived in isolated refuges and there was higher atmospheric circulation.
The Amazon forest was reduced to a small refuge and almost wiped out.
By contrast, 6,000 to 7,000 years ago was what geographers term the mid-Holocene
thermal optimum, when global mean temperatures were some two to three
degrees centigrade warmer than present. With warmer climates comes increased
precipitation and in the Holocene optimum global net precipitation was
nine per cent higher. So, for instance, the Sahara desert, which was considerably
more extensive during the Pleistocene ice ages, effectively did not exist.
The Savannah which replaced it was hospitable to human life and it was
only with the general cooling after the Holocene optimum that the Sahara
grew to its present extent. There were some areas of increase aridity,
such as Turkey and the Rockies but in general the Holocene optimum meant
a more fertile and productive earth.
We
have nothing to fear from nature with global warming. Some areas of productive
farmland would be lost but they would be more than replaced by new areas
for agriculture. A flourishing Sahara desert surely would be a good thing
on a global scale. So just as scare stories about Britain
acquiring a Mediterranean climate can make us say roll on global
warming, so does everything history has to tell us about the state
of a warmer world. But what about local extremes of climate that the environmental
disaster lobby predict? To look at this issue we first have to understand
the causes of climate change.
The
accepted theory of climate change shows that in palaeo-climates the carbon
dioxide content of the atmosphere broadly responds to global temperature
change. Note the chain of causality: historically, carbon dioxide concentrations
have followed climate change, rather than forcing change. As important
as this observation, is that even though this is true for the big picture
on the scale of tens of thousands of years over small time intervals of
a few thousand years, the temperature record and carbon dioxide record
can be moving in opposite directions. This needs to be borne in mind when
meteorologists are making their observations over periods of decades and
at best hundreds of years (although without the global coverage of instrumentation).
So
for scientists–the sceptics - who reject the notion
of anthropogenic induced global warming, there is plenty to get their
teeth into. Certainly we should be sceptical of assertions that extreme
weather events experienced today are linked to rising carbon dioxide levels.
Assuming that increased concentrations of carbon dioxide can force warming,
will a warmer or a warming world be more unstable even if it is overall
perhaps more hospitable to human life?
Extreme global events
It is often argued that the very rate of global climate change is the
problem and likely to cause extreme global events. Research into extreme
geological events is certainly some of the most exciting research being
undertaken at the present time: the idea that huge tsunami waves would
have battered the eastern seaboard of America triggered by submarine slumping
in the Canary Islands; the possibility of widespread volcanic dust in
the western US and the implications for large-scale volcanism; and of
course the realisation that a comet impact probably caused the extinction
of the dinosaurs. The projected rise in global mean temperature itself
might not be so alarming but extreme events could be. In this category
of extreme events we have to include changes whose very speed is problematic
rather than necessarily the magnitude of the change, which if slower could
be accommodated.
Now
the rate of change/extreme global events argument must
be treated with some caution. To begin with, the global climate in the
past has clearly changed far more than the projected changes of the Intergovernmental
Panel on Climate Change. Secondly most climate models which look at the
consequences of doubling carbon dioxide do just that. At year X they double
carbon dioxide content of the atmosphere. It can hardly be surprising
that if you suddenly change the inputs into a computer programme, you
will get great lurches in the predictions made by the programme, which
have no bearing on reality.
The
extreme events case has most recently been argued by the chief
scientific adviser to the British Government, Sir Robert May FRS. One
of the problems raised is the increased likelihood of tropical hurricanes
in a warmer world. Models have been constructed which back up this idea.
The general case for more violent atmospheric circulation globally is
not borne out by the historical evidence, again from deep ice cores: these
indicate more stability in a warmer world. The chief scientific adviser
also raised the possibility that the Gulf Stream, responsible for bringing
warmth to north-west Europe, could be shut off. This is of course scary
stuff for while the world warms Britain would turn into a sub-Arctic wasteland.
The argument for this is based on the idea that increased precipitation
in the North Atlantic region and increased fresh water run-off, would
reduce the salinity of surface water. Water will therefore be less dense
and would not sink so readily. The geological records suggest the opposite
happened– warmer climates meant stronger deep water formation. (The
initiation of northern hemisphere glaciation, M E Raymo, Annual Review
of Earth Planetary Science, 1994)
Contribution of deforestation
to global warming
Tropical moist lowlands forests and especially the largest area still
remaining, the Amazon rainforest, have become a particular focus of attention.
Not just for the question of the loss of biodiversity but also for the
impact of changes in land use on net greenhouse emissions. Satellite estimates
of the rate of tropical land use change produced in the early eighties,
(later found to be gross exaggerations), contributed to fears that were
raised as the global warming debate was getting under way. Satellite measurements
of average yearly deforestation were later revised down from 80,000 square
kilometres to 20,000 square kilometres.
The
contribution of the Amazon towards global net greenhouse emissions is
often misunderstood. Reduction in the amount of carbon dioxide absorbed
by forests as a result of deforestation has the effect of increasing the
amount of solar radiation reflected, so lowering temperatures, at the
same time this contribution is counterbalanced by increased aridity.
The
contributions of land use changes to global warming need to be put into
perspective. It has been calculated that the contribution of changes in
land use to net greenhouse emissions, calculated in millions of tonnes
of carbon dioxide is, 4,100 globally, 1,800 for the whole of South America.
This compares with 22,300 million tonnes of worldwide industrial emissions.
The contribution of deforestation in the Amazon region is comparatively
very small.
Why do we fear global
warming?
Why is global warming seen as such a problem?
In the first place people and human societies are seen as likely victims
of change, unable to adapt, never mind thrive in or modify a changing
natural world. This is most evident in the discussion of the developing
world. 85 per cent of Bangladeshs population depends on agricultural
production for a livelihood and the coastal regions–which could
be flooded if warming causes sea levels to rise appreciably and no defences
were erected - are the most fertile. The argument that global warming
would be a disaster for Bangladesh is easily made. But what this argument
reveals is the view that in 100 years time Bangladesh will not have moved
beyond the kind of economy it is today–an incredibly static view
of development. It is at this juncture that the issues of global warming
and population control meet. Global warming, so the argument goes, is
an additional stress on the system, already under pressure from population
growth in a world of finite resources. This is argued in the recent joint
publication by The Royal Society and the US National Academy of Sciences,
Towards sustainable consumption. If we can simply argue against the notion
that resources are finite and what is needed is more development and not
less to end poverty, this also points the way to addressing the problems
that could result from global warming in some areas. We must promote the
development of Bangladesh, not check it.
Global warming is also widely taken to be a metaphor for the way we are
messing up the planet. As such, it must be condemned. A warmer world would,
on balance, be a good thing. As the American writer Gregg Easterbrook
has argued: the idea that clumsy tinkering with the environment
has done something useful-that we benefit from pollution!-is almost too
peculiar for polite discourse. That phrase is indicative of the
way the issue is discussed–carbon dioxide is no more a pollutant
than fresh water or sunlight.

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