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This article was published 27/1/2013 (1609 days ago), so information in it may no longer be current.
WASHINGTON -- Heat rising up from cities such as New York, Paris and Tokyo might be remotely warming up winters as far away as Manitoba, North Dakota and Alaska, a surprising study theorizes.
In an unusual twist, that same urban heat from buildings and cars may be slightly cooling the autumns in much of the Western United States, Eastern Europe and the Mediterranean, according to the study published Sunday in the scientific journal Nature Climate Change.
Meteorologists have long known cities are warmer than rural areas, with the heat of buildings and cars, along with asphalt and roofs that absorb heat. That's called the urban heat island effect, and it's long been thought the heat stayed close to the cities.
But the study, based on a computer model and the Northern Hemisphere, now suggests the heat does something else, albeit indirectly. It travels about 800 metres up into the air and then its energy changes the high-altitude currents in the atmosphere that dictate prevailing weather.
"Basically, it changes the flow," said Guang Zhang of the Scripps Institution of Oceanography in La Jolla, Calif. He wrote the paper with Aixue Hu at the National Center for Atmospheric Research in Boulder, Colo.
This doesn't change overall global temperature averages significantly, unlike man-made greenhouse gases that cause global warming. Instead, it redistributes some of the heat, the scientists said.
The changes seem to vary with the seasons and by region because of the way air currents flow at different times of the year. During the winter, the jet stream is altered and weakened, keeping cold air closer to the Arctic Circle and from dipping down as sharply, Hu explained.
The computer model showed parts of Siberia and northwestern Canada may get, on average, an extra 0.8 to one degree Celsius during the winter, which "may not be a bad thing," Zhang said. The effect isn't quite as much in Manitoba and northern North Dakota, where temperatures might be about half a degree warmer (0.3 C).
In contrast, Europe and the Pacific Northwest are cooled slightly in the winter from this effect. The jet-stream changes prevent weather systems from bringing warmer air from the Atlantic to Europe and from the Pacific to the U.S. Northwest, thus cooling those areas a bit, he said.
The biggest cooling occurs in the fall, but Hu said he's not quite sure why that happens.
Several outside scientists said they were surprised by the study results, calling the work "intriguing" and "clever." But they said it would have to be shown in more than one computer model and in repeated experiments before they could accept this theory.
-- The Associated Press