Читать книгу High Tide: How Climate Crisis is Engulfing Our Planet - Mark Lynas - Страница 7

As it happens, such evidence is indeed available for the UK. To find out more, I went to visit the climatologist Dr Tim Osborn at the Climatic Research Unit (CRU), part of the University of East Anglia. It was almost two years to the day after the start of the autumn 2000 disaster, and there was a hint of winter in the air as the London train sped through the Essex town of Colchester, past the River Stour saltmarshes and on through the flat Norfolk fenlands to Norwich.

As so often, Osborn confounded my expectations. No white lab coat for him: instead, a youngish, fair-haired man in shorts, trainers and a red golfing T-shirt was leaning over the balcony three floors above as I arrived at the round, glass-fronted CRU building.

‘Hello! Come on up,’ he shouted as I climbed the stairs. His room was strewn with back copies of the International Journal of Climatology and meteorology books, as well as sheafs of paper – many covered with impenetrable algebraic scribbles.

‘Sorry about the mess,’ he said as I sat down on a free chair. Then he swivelled his own chair round to face the computer screen. ‘Now, have a look at this.’

Osborn has spent years analysing nearly half a century of rainfall statistics. From a damp day in 1960s Blackpool to a torrential summer downpour in 1990s Devon, all these records were fed into his number-crunching computer. When spat out the other end into a series of graphs, these statistics – rather than just showing the usual random vagaries of the British weather – showed that something very unusual was going on. In fact the trend was so clear that even Osborn himself was ‘surprised’ by what it revealed.

What Osborn discovered was that over recent decades heavy winter downpours have indeed increased dramatically. ‘Over the period from the 1960s to the mid-1990s there was a doubling of the amount of rain that came in the “heavy category” in winter,’ he explained. ‘So in the 1960s something like seven or eight per cent of each winter’s rainfall came from what we call the “heavy” events, whilst by the mid-1990s that had increased to about fifteen per cent.’⁶

With more rain falling in a short time, river systems were unable to cope – and floods were the inevitable result. What’s more, this heavier winter rainfall was directly related to rising atmospheric temperatures.

Straightforward atmospheric physics suggests this could be the global warming ‘smoking gun’. The relationship between temperature and the air’s capacity to hold water vapour is not linear – in fact the air can hold proportionally more water as temperature rises.⁷ So in a given ‘precipitation event’, whether it is snow, hail or rain, more water is available to fall out of the sky over the same short period of time.

This is exactly what seems to be happening in Britain: as a result of global warming, more warm, saturated air rushes in from the Atlantic, causing stronger storms and heavier rainfall. As a result, the probability of heavy rainfall has doubled over the last thirty-five to forty years in southeast England, according to observations and analysis conducted by Osborn and his CRU colleague Mike Hulme.⁸

These aren’t one-off downpours, either. The frequency of prolonged five-day heavy rainfall events has also been increasing. In Scotland floods have been getting far more frequent over the last few decades, whilst in England and Wales there have been four major floods in the last twelve winters: 1989/90, 1993/94, 1994/95 and, of course, 2000/01.⁹ The match for 2000 isn’t perfect because the worst flooding came during the autumn – but the floods also lasted right through until January, just as the trend would suggest.

Osborn’s work also coincides with evidence from other parts of the world. Study after study has come to the same conclusion: that throughout Earth’s mid-latitudes, rainfall is getting heavier and more destructive. There has been a steadily increasing rainfall trend in the United States through the twentieth century, and much of that increase has come in the heaviest downpours. A number of catastrophic floods in recent years – most notably the Mississippi floods of 1993, the New England floods of 1997 and the winter floods of 1997 in the Pacific northwest and California – seem to show the shape of things to come.¹⁰

Scientists have reached a similar conclusion in Europe,¹¹ whilst in Australia rainfall totals are also rising steadily.¹² This might seem to be a good thing in a continent often afflicted by drought – but again, much of the increase has come in the heaviest deluges, which are less likely to soak productively into farmland, and more likely to run quickly off the land in destructive torrents, taking the fertile topsoil with them.

One study looking specifically at large river basins – such as the Yangtze in China and the Danube in Europe – confirms what many people have long suspected: that big floods are indeed getting more frequent. In fact, sixteen of twenty-one ‘great floods’ during the twentieth century have occurred since 1953, and in the planetary mid-latitudes seven out of eight have also occurred in the second half of the century.¹³ UK-based researchers have also identified a near-global trend towards heavier rain and floods.¹⁴

In the most comprehensive survey of all, the Intergovernmental Panel on Climate Change (IPCC) confirmed that rainfall was getting heavier and more extreme in the United States, Canada, Switzerland, Japan, the UK, Norway, South Africa, northeast Brazil and the former USSR.¹⁵

This hasn’t affected everywhere: some places have got drier, such as the Sahel in Africa and northern China. But almost the whole of the Earth’s mid-latitudes has been affected, and as Osborn told me, ‘if there’s something coherent going on at all the mid-latitudes, then there must be something virtually global scale driving it’. Computer models of global warming have long illustrated this effect, and now it seems to be showing up in the real world, just as many scientists – including Osborn himself – have long predicted.