The Unusual Midwinter Warming in the Southern Hemisphere Stratosphere 2002: A Comparison to Northern Hemisphere Phenomena

Kirstin Krüger Institut für Meteorologie, Freie Universität Berlin, Berlin, Germany

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Barbara Naujokat Institut für Meteorologie, Freie Universität Berlin, Berlin, Germany

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Karin Labitzke Institut für Meteorologie, Freie Universität Berlin, Berlin, Germany

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Abstract

A strong midwinter warming occurred in the Southern Hemisphere (SH) stratosphere in September 2002. Based on experiences from the Northern Hemisphere (NH), this event can be defined as a major warming with a breakdown of the polar vortex in midwinter, which has never been detected so far in the SH since observations began at the earliest in the 1940s. Minor midwinter warmings occasionally occurred in the SH, but a strong interannual variability, as is present in winter and spring in the NH, has been explicitly associated with the spring reversals.

A detailed analysis of this winter reveals the dominant role of eastward-traveling waves and their interaction with quasi-stationary planetary waves forced in the troposphere. Such wave forcing, finally leading to the sudden breakdown of the vortex, is a familiar feature of the northern winter stratosphere. Therefore, the unusual development of this Antarctic winter is described in the context of more than 50 Arctic winters, concentrating on winters with similar wave perturbations. The relevance of preconditioning of major warmings by traveling and quasi-stationary planetary waves is discussed for both hemispheres.

* Current affiliation: Alfred Wegener Institute for Polar and Marine Research, Potsdam, Germany

Corresponding author address: Dr. Kirstin Krüger, Alfred Wegener Institute for Polar and Marine Research, P.O. Box 60 01 49, Telegrafenberg A43, 14401 Potsdam, Germany. Email: kkrueger@awi-potsdam.de

Abstract

A strong midwinter warming occurred in the Southern Hemisphere (SH) stratosphere in September 2002. Based on experiences from the Northern Hemisphere (NH), this event can be defined as a major warming with a breakdown of the polar vortex in midwinter, which has never been detected so far in the SH since observations began at the earliest in the 1940s. Minor midwinter warmings occasionally occurred in the SH, but a strong interannual variability, as is present in winter and spring in the NH, has been explicitly associated with the spring reversals.

A detailed analysis of this winter reveals the dominant role of eastward-traveling waves and their interaction with quasi-stationary planetary waves forced in the troposphere. Such wave forcing, finally leading to the sudden breakdown of the vortex, is a familiar feature of the northern winter stratosphere. Therefore, the unusual development of this Antarctic winter is described in the context of more than 50 Arctic winters, concentrating on winters with similar wave perturbations. The relevance of preconditioning of major warmings by traveling and quasi-stationary planetary waves is discussed for both hemispheres.

* Current affiliation: Alfred Wegener Institute for Polar and Marine Research, Potsdam, Germany

Corresponding author address: Dr. Kirstin Krüger, Alfred Wegener Institute for Polar and Marine Research, P.O. Box 60 01 49, Telegrafenberg A43, 14401 Potsdam, Germany. Email: kkrueger@awi-potsdam.de

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