Weather from the Stratosphere?-Reference-Cited by-同舟云学术

Weather from the Stratosphere?

Published:2003-07-18 Issue:5631 Volume:301 Page:317-319
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Baldwin Mark P.¹,Thompson David W. J.²,Shuckburgh Emily F.³,Norton Warwick A.⁴,Gillett Nathan P.⁵

Affiliation:

1. M. P. Baldwin is at NorthWest Research Associates, Bellevue, WA 98007, USA.

2. D. W. J. Thompson is in the Department of Atmospheric Science, Colorado State University, Fort Collins, CO 80523, USA.

3. E. F. Shuckburgh is in the Department of Applied Mathematics and Theoretical Physics, University of Cambridge, Cambridge CB3 0WA, UK.

4. W. A. Norton is in the Department of Atmospheric, Oceanic, and Planetary Physics, University of Oxford, Oxford OX1 3PU, UK.

5. N. P. Gillett is in the School of Earth and Ocean Sciences, University of Victoria, Victoria, BC V8W 3P6, Canada.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference13 articles.

1. The Role of the Stratosphere in Tropospheric Climate Whistler British Columbia Canada 29 April to 2 May 2003. For abstracts and presentations see www.atm.damtp.cam.ac.uk/shuckburgh/whistler.

2. McIntyre M. E., Palmer T. N., Nature305, 593 (1983).

3. In response to the strong equator-to-pole gradient of solar heating that prevails during winter polar temperatures drop to below −70°C in the stratosphere and the high-latitude winds form a “polar vortex ” with winds blowing from west to east.

4. Stratospheric Harbingers of Anomalous Weather Regimes

5. The Arctic oscillation signature in the wintertime geopotential height and temperature fields

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