US, Mediterranean face extreme warming: study

Once the world has warmed by two degrees Celsius, top temperatures in hot spots like the United States and Mediterranean basin would jump at least 3.0C

Once the world as a whole has warmed by two degrees Celsius, top temperatures in the United States and Mediterranean basin will have climbed by even more, according to a study released Wednesday.

A global 2C (3.6 Fahrenheit) rise above mid-19th century levels would mean a jump of at least 3.0C (5.4F) in maximum daytime temperatures in these regional hot spots—deep into the red zone of dire climate impacts, said the study.

Central Brazil can also look forward to a bigger-than-average increase, with summertime peaks rising by 3.5C.

Moreover, no matter how quickly humanity reduces the that drive warming, the gaps will remain just as big.

“These relationships hold true regardless of what emissions pathway you take,” Sonia Seneviratne, a professor at ETH Zurich’s Institute for Atmospheric and Climate Science, told AFP by phone.

“If our aim is to limit summer temperature extremes in the Mediterranean region, for example, to 2C, then the global temperature must rise no more than 1.4C.”

The study, published in Nature, looked at projections in each region for the evolution of annual maximum and minimum daytime temperatures.

In 2010, the world’s nations set a goal of capping average planet-wide warming to 2C, a hugely daunting task.

But a crescendo of extreme weather—US government scientists confirmed today that 2015 was “by far” the hottest year on record—and new studies suggest that even this ambitious goal may be inadequate.

A more recent global climate agreement, inked by 195 countries in Paris in December, set a new target of “well below 2C”.

Earth has already heated up by nearly 1.0C. Scientist do not know when it might pierce the 2C cap, but many acknowledge that the chances of staying under it are not good.

Regional hot spots

There are several explanations for the gap between global averages and “hot spot” regions, Seneviratne explained.

One is the simple fact that temperatures above the oceans—which cover more than 70 percent of the planet’s surface—are significantly cooler, bringing down the average.

Beyond that, however, there are local factors—the impact of parched soils, loss of heat-reflecting snow—that make some land areas even hotter.

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