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Different impact of central Pacific and eastern Pacific El Niño on the duration of sudden stratospheric warming
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  • Original Paper
  • Open Access
  • Published: 29 April 2017

Different impact of central Pacific and eastern Pacific El Niño on the duration of sudden stratospheric warming

  • Yuanpu Li1 &
  • Wenshou Tian1 

Advances in Atmospheric Sciences volume 34, pages 771–782 (2017)Cite this article

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Abstract

The NCEP–NCAR reanalysis dataset and the HadISST dataset (1959–2014) are used to analyze the impact of two types of El Niño events, i.e., eastern Pacific El Niño (EP-El Niño) and central Pacific El Niño (CP-El Niño) events, on the duration of major and minor sudden stratospheric warmings (SSWs) in Northern Hemisphere winter (November to February). Although the frequency of major and minor SSWs during different types of El Niño shows no distinct differences, the duration of both major and minor SSWs during CP-El Niño is shorter than that during EP-El Niño. The spatial distribution of geopotential height anomalies preceding major SSWs resembles the western Pacific (WP) teleconnection pattern, while the spatial distribution of geopotential height anomalies preceding minor SSWs bears similarity to the Pacific–North America (PNA) teleconnection pattern. An enhancement of the strength of both wavenumber 1 and wavenumber 2 is found before major SSWs. Before minor SSWs, wavenumber 1 is also strengthened, but wavenumber 2 is weakened. The analysis also reveals that EP-El Niño tends to induce positive phases of PNA and WP teleconnections, while CP-El Niño induces negative-phase WP teleconnection. As the positive phases of the PNA and WP teleconnections are related to the strengthening of wavenumber 1, EP-El Niño causes an enhancement of wavenumber 1 in the high-latitude upper troposphere and an enhancement of the upward wave flux in the high-latitude stratosphere, accompanied by a negative anomaly in Eliassen–Palm flux divergence in the subpolar stratosphere, which accounts for the longer SSW duration during EP-El Niño than during CP-El Niño.

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Acknowledgments

We are grateful to the agencies for providing the datasets used in this study. This work was supported by the National Natural Science Foundation of China (Grant Nos. 41225018 and 41575038).

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Authors and Affiliations

  1. College of Atmospheric Science, Lanzhou University, Lanzhou, 730000, China

    Yuanpu Li & Wenshou Tian

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  1. Yuanpu Li
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  2. Wenshou Tian
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Correspondence to Wenshou Tian.

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Open Access. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons. org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.

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Open Access. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.

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Cite this article

Li, Y., Tian, W. Different impact of central Pacific and eastern Pacific El Niño on the duration of sudden stratospheric warming. Adv. Atmos. Sci. 34, 771–782 (2017). https://doi.org/10.1007/s00376-017-6286-0

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  • Received: 23 November 2016

  • Revised: 13 February 2017

  • Accepted: 27 February 2017

  • Published: 29 April 2017

  • Issue Date: June 2017

  • DOI: https://doi.org/10.1007/s00376-017-6286-0

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Key words

  • SSW
  • teleconnection
  • El Niño
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