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Schnadt & Dameris 2003
Schnadt, C. and Dameris, M. (2003). Relationship between North Atlantic Oscillation changes and stratospheric ozone recovery in the Northern Hemisphere in a chemistry-climate model. Geophysical Research Letters 30: doi: 10.1029/2003GL017006. issn: 0094-8276.

The relationship between North Atlantic Oscillation (NAO) changes and northern stratospheric ozone recovery in the near future is investigated using four timeslice scenarios (1960, 1980, 1990, 2015) of the chemistry-climate model ECHAM4.L39(DLR)/CHEM. A wintertime NAO index composite study of the scenario 1990 and of the ECMWF reanalyses shows the typical NAO patterns: in the positive phase the stratospheric polar vortex is stronger and colder than in the negative phase. In the troposphere, the positive phase is marked by increased variance across the North Atlantic stormtrack whereas the negative phase is suggestive of blocking. Consistently, vertical stationary (transient) wave propagation is reduced (enhanced) in the positive phase. The model NAO index decreases significantly from 1990 to 2015. This coincides with enhanced vertical stationary wave propagation and a dynamical heating of the northern polar stratosphere. Thus, tropospheric circulation changes might influence stratospheric dynamics and hence northern hemisphere ozone evolution.

BACKGROUND DATA FILES

Abstract

Keywords
Meteorology and Atmospheric Dynamics, Stratosphere/troposphere interactions, Meteorology and Atmospheric Dynamics, Middle atmosphere dynamics (0341, 0342), Atmospheric Composition and Structure, Middle atmosphere--constituent transport and chemistry
Journal
Geophysical Research Letters
http://www.agu.org/journals/gl/
Publisher
American Geophysical Union
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