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GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L12706, doi:10.1029/2008GL033573, 2008

Impact of the stratosphere on tropospheric climate change

Michael Sigmond

Department of Physics, University of Toronto, Toronto, Ontario, Canada


John F. Scinocca

Canadian Centre for Climate Modelling and Analysis, Meteorological Service of Canada, Victoria, British Columbia, Canada


Paul J. Kushner

Department of Physics, University of Toronto, Toronto, Ontario, Canada


Abstract

The atmospheric circulation response to CO2 doubling in various versions of an atmospheric general circulation model (AGCM) without a well-resolved stratosphere (“low-top” model), is compared to the response in a version of the same AGCM with a well-resolved stratosphere (“high-top” model). The doubled CO2 response of the “best-tuned” (i.e. operational) low-top model version is significantly different from that in the best-tuned high-top model version. Additional experiments show that this difference is not caused by the model lid height, but instead can be mainly attributed to differences in the settings of parameterized orographic gravity-wave drag which control the strength of the zonal wind in the mid- to high-latitude lower stratosphere and the mean sea-level pressure distribution. These findings suggest a link between the strength of the winds in the mid- to high-latitude lower stratosphere and tropospheric annular mode responses, and have implications for how to proceed with high-top low-top model intercomparisons.

Received 7 February 2008; accepted 15 May 2008; published 24 June 2008.

Keywords: stratosphere-troposphere coupling; climate change.

Index Terms: 3362 Atmospheric Processes: Stratosphere/troposphere interactions; 1610 Global Change: Atmosphere (0315, 0325); 1620 Global Change: Climate dynamics (0429, 3309).

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Citation: Sigmond, M., J. F. Scinocca, and P. J. Kushner (2008), Impact of the stratosphere on tropospheric climate change, Geophys. Res. Lett., 35, L12706, doi:10.1029/2008GL033573.