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Part of the report’s job is to consider studies of the speed of change so far. Warming seems to be accelerating somewhat. Eleven out of the dozen years from 1995-2006 were among the 12 hottest years since 1850, when temperatures were first widely recorded. So the estimate for the average increase in global temperature for the past century, which the third assessment report put at 0.6C, has now risen to 0.74C.
The sea level, which rose on average by 1.8mm a year in 1961-2003, went up by an average of 3.1mm a year between 1993-2003. The numbers are still small, but the shape of the curve is worrying. And because the deadline for scientific papers to be included in the IPCC’s report was some time ago, its deliberations have excluded some alarming recent studies on the acceleration of glacier melt in Greenland.
Some trends now seem clear. North and South America and northern Europe are getting wetter; the Mediterranean and southern Africa drier. Westerly winds have strengthened since the 1960s. Droughts have got more intense and longer since the 1970s. Heavy rainfall, and thus flooding, has increased. Arctic summertime sea ice is decreasing by just over 7% a decade.
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The other part of the report’s job is to make predictions about what will happen to the climate. In this, it illustrates a curious aspect of the science of climate change. Studying the climate reveals new, little-understood, mechanisms: as temperatures warm, they set off feedback effects that may increase, or decrease, warming. So predictions may become less, rather than more, certain. Thus the IPCC’s range of predictions of the rise in the temperature by 2100 has increased from 1.4-5.8C in the 2001 report to 1.1-6.4C in this report.
That the IPCC should end up with a range that vast is not surprising given the climate’s complexity. But it leaves plenty of scope for argument about whether it’s worth trying to do anything about climate change.
The Economist
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