Simulation of recent northern winter climate trends by greenhouse-gas forcing

Drew T. Shindell (), Ron L. Miller, Gavin A. Schmidt and Lionel Pandolfo
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Drew T. Shindell: NASA Goddard Institute for Space Studies
Ron L. Miller: Center for Climate Systems Research, Columbia University
Gavin A. Schmidt: NASA Goddard Institute for Space Studies
Lionel Pandolfo: University of British Columbia

Nature, 1999, vol. 399, issue 6735, 452-455

Abstract: Abstract The temperature of air at the Earth's surface has risen during the past century1, but the fraction of the warming that can be attributed to anthropogenic greenhouse gases remains controversial. The strongest warming trends have been over Northern Hemisphere land masses during winter, and are closely related to changes in atmospheric circulation. These circulation changes are manifested by a gradual reduction in high-latitude sea-level pressure, and an increase in mid-latitude sea-level pressure associated with one phase of the Arctic Oscillation (a hemisphere-scale version of the North Atlantic Oscillation)2. Here we use several different climate-model versions to demonstrate that the observed sea-level-pressure trends, including their magnitude, can be simulated by realistic increases in greenhouse-gas concentrations. Thus, although the warming appears through a naturally occurring mode of atmospheric variability, it may be anthropogenically induced and may continue to rise. The Arctic Oscillation trend is captured only in climate models that include a realistic representation of the stratosphere, while changes in ozone concentrations are not necessary to simulate the observed climate trends. The proper representation of stratospheric dynamics appears to be important to the attribution of climate change, at least on a broad regional scale.

Date: 1999
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DOI: 10.1038/20905

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