Journal of Geophysical Research: Atmospheres

Why might stratospheric sudden warmings occur with similar frequency in El Niño and La Niña winters?

Authors

  • C. I. Garfinkel,

    Corresponding author
    1. Department of Earth and Planetary Science, Johns Hopkins University, Baltimore, Maryland, USA
      Corresponding author: C. I. Garfinkel, Department of Earth and Planetary Science, Johns Hopkins University, Baltimore, MD 21209, USA. (cig4@jhu.edu)
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  • A. H. Butler,

    1. Climate Prediction Center, NCEP, NOAA, Camp Springs, Maryland, USA
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  • D. W. Waugh,

    1. Department of Earth and Planetary Science, Johns Hopkins University, Baltimore, Maryland, USA
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  • M. M. Hurwitz,

    1. Goddard Earth Sciences Technology and Research, Morgan State University, Baltimore, Maryland, USA
    2. NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
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  • L. M. Polvani

    1. Department of Applied Physics and Applied Mathematics and Department of Earth and Environmental Sciences, Columbia University, New York, New York, USA
    2. Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York, USA
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Corresponding author: C. I. Garfinkel, Department of Earth and Planetary Science, Johns Hopkins University, Baltimore, MD 21209, USA. (cig4@jhu.edu)

Abstract

[1] The effect of El Niño-Southern Oscillation (ENSO) on the frequency and character of Northern Hemisphere major mid-winter stratospheric sudden warmings (SSWs) is evaluated using a meteorological reanalysis data set and comprehensive chemistry-climate models. There is an apparent inconsistency between the impact of opposite phases of ENSO on the seasonal mean vortex and on SSWs: El Niño leads to an anomalously warm, and La Niña leads to an anomalously cool, seasonal mean polar stratospheric state, but both phases of ENSO lead to an increased SSW frequency. A resolution to this apparent paradox is here proposed: the region in the North Pacific most strongly associated with precursors of SSWs is not strongly influenced by El Niño and La Niña teleconnections. In the observational record, both La Niña and El Niño lead to similar anomalies in the region associated with precursors of SSWs and, consistent with this, there is a similar SSW frequency in La Niña and El Niño winters. A similar correspondence between the penetration of ENSO teleconnections into the SSW precursor region and SSW frequency is found in the comprehensive chemistry-climate models. The inability of some of the models to capture the observed relationship between La Niña and SSW frequency appears related to whether the modeled ENSO teleconnections result in extreme anomalies in the region most closely associated with SSWs. Finally, it is confirmed that the seasonal mean polar vortex response to ENSO is only weakly related to the relative frequency of SSWs during El Niño and La Niña.

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