The Water Boom Is Over
Global freshwater supplies could start to determine whether or not we can feed ourselves.
George Monbiot. Published in the Guardian 10th October 2006.
It looks dull, almost impenetrable in places. But if its findings are verified, it could turn out to be the most important scientific report published so far this year. In this month's edition of the Journal of Hydrometeorology is a paper written by scientists at the Met Office, which predicts future patterns of rainfall and evaporation(1).
Those who dispute that climate change is taking place, such as Melanie Phillips of the Daily Mail, like to point out that the predicted effects of global warming rely on computer models, rather than "observable facts"(2). That's the problem with the future - you can't observe it. But to have any hope of working out what might happen, you need a framework of understanding. It's either this or the uninformed guesswork that Philips seem to prefer.
The models can be tested by means of what climate scientists call backcasting – seeing whether or not they would have predicted changes which have already taken place. The global climate model used by the Met Office still needs to be refined. While it tracks past temperature changes pretty closely, it does not accurately backcast the drought patterns in every region. But it correctly reproduces the total global water trends over the past 50 years. When the same model is used to forecast the pattern over the 21st Century, it uncovers "a net overall global drying trend" if greenhouse gas emissions are moderate or high. "On a global basis, drought events are slightly more frequent and of much longer duration by the second half of the 21st century relative to the present day."(3) In these dry, stodgy phrases, we find an account of almost unimaginable future misery.
Many parts of the world, for reasons which have little to do with climate change, are already beginning to lose their water. In When the Rivers Run Dry, Fred Pearce, who is New Scientist's environment consultant, travels around the world trying to assess the state of our water resources(4). He finds that we survive today as a result of borrowing from the future.
The great famines predicted for the 1970s were averted by new varieties of rice, wheat and maize, whose development is known as the "green revolution". They produce tremendous yields, but require plenty of water. This has been provided by irrigation, much of which uses undergound reserves. Unfortunately, many of them are being exploited much faster than they are being replenished. In India, for example, some 250 cubic kilometres (a cubic kilometre is a billion cubic metres or a trillion litres) are extracted for irrigation every year, of which about 150 are replaced by the rain. "200 million people [are] facing a waterless future. The groundwater boom is turning to bust and, for some, the green revolution is over."
In China, 100 million people live on crops grown with underground water that is not being refilled: water tables are falling fast all over the North China plain. Many more rely on the Huang He (the Yellow River), which already appears to be drying up as a result of abstraction and possibly climate change. Ninety percent of the crops in Pakistan are watered by irrigation from the Indus. Almost all the river's water is already diverted into the fields - it often fails now to reach the sea. The Ogallala aquifer which lies under the western and south western United States, and which has fed much of the world, has fallen by 30 metres in many places. It now produces half as much water as it did in the 1970s.
All this was known before the new paper was published. While climate scientists have been predicting for some time that the wet parts of the world are likely to become wetter and the dry parts drier, they had assumed that overall rainfall would rise, as higher temperatures increase evaporation. At the same time - and for the same reason – soils could become drier. It was unclear what the net effects would be. But the new paper's "drought index" covers both rainfall and evaporation: overall, the world becomes drier.
Even this account – of rising demand and falling supply – does not tell the whole grim story. Roughly half the world's population lives within 60 kilometres of the coast. Eight of the ten largest cities on earth have been built beside the sea. Many of them rely on underground lenses of fresh water, effectively floating, within the porous rocks, on salt water which has soaked into the land from the sea. As the fresh water is sucked out, the salt water rises and can start to contaminate the aquifer. This is already happening in hundreds of places. The worst case is the Gaza strip, which relies entirely on underground water which is now almost undrinkable. As the sea level rises as a result of climate change, salt pollution in coastal regions is likely to accelerate(5,6).
As these two effects of climate change - global drying and rising salt pollution - run up against the growing demand for water, and as irrigation systems run dry or become contaminated, the possibility arises of a permanent global food deficit. Even with a net food surplus, 800 million people are malnourished. Nothing I could write would begin to describe what a world in deficit – carrying 9 billion people – would look like.
There are four possible means of adapting to this crisis. One is to abandon regions that are drying up and shift production to the wettest parts of the world – the Amazon and Congo Basins, for example. But as these are generally the most forested places, this will lead to a great acceleration of climate change, and of the global drying it's likely to cause, as the carbon in the trees is turned to carbon dioxide. Another is to invest in desalination plants. But even the new desalination technologies produce expensive water, and they use a great deal of energy. Again this means more global warming.
Another is to shift water, on a massive scale, to the drying lands. But vast hydro-engineering projects have seldom succeeded in helping the poor. Giant dams and canals - like the Narmada system in India, the Three Gorges in China and Colonel Gaddafi's "Great Man-made River" - are constructed at stupendous cost. Then, when no further glory can be extracted by the government officials and companies who built them, the fiddly work of ensuring the water reaches the poor is forgotten, and all the money is wasted. As Fred Pearce shows, perhaps the best method, which in the past has kept cities alive even in the Negev desert, is the small-scale capture of rainwater in ponds and tanks(7).
But to stand a high chance of averting this catastrophe, we must ensure that the drying doesn't happen. The predictions in the new paper refer to global warming in the middle or at the high end of the expected range. Beneath that point - 2C of warming or so - a great global drying is less likely to occur. As the figures I've published show, to keep the temperature rise below this level requires a global cut in carbon emissions of 60% by 2030 - which means a 90% reduction in rich nations like the United Kingdom(8). It sounds impossible. But then you consider the alternative.
George Monbiot's book Heat: how to stop the planet burning is published by Penguin.
1. EJ Burke, SJ Brown, and N Christidis, October 2006. Modeling the Recent Evolution of Global Drought and Projections for the Twenty-First Century with the Hadley Centre Climate Model. Journal of Hydrometeorology vol 7, no 5, pp 1113-1125.
2. Eg Melanie Phillips, 12th January 2004. Global Warming Or Global Fraud? Daily Mail.
3. EJ Burke, SJ Brown, and N Christidis, ibid.
4. Fred Pearce, 2006. When the Rivers Run Dry. Eden Books, Transworld, London.
5. VEA Post, 2005. Fresh and Saline Groundwater Interaction in Coastal Aquifers: is our technology ready for the problems ahead? Hydrogeology Journal, vol 13, pp 120-123.
6. Gualbert H.P. Oude Essink, 2001. Improving fresh groundwater supply: problems and solutions.
Ocean & Coastal Management vol 44, pp 429-449.
7. Fred Pearce, ibid.
8. George Monbiot, 2006. Heat: how to stop the planet burning. Penguin, London.