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Persistent shift of the Arctic polar vortex towards the Eurasian continent in recent decades

Nature Climate Change volume 6, pages 1094–1099 (2016)Cite this article

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Abstract

The wintertime Arctic stratospheric polar vortex has weakened over the past three decades, and consequently cold surface air from high latitudes is now more likely to move into the middle latitudes1,2,3,4,5. However, it is not known if the location of the polar vortex has also experienced a persistent change in response to Arctic climate change and whether any changes in the vortex position have implications for the climate system. Here, through the analysis of various data sets and model simulations, we show that the Arctic polar vortex shifted persistently towards the Eurasian continent and away from North America in February over the past three decades. This shift is found to be closely related to the enhanced zonal wavenumber-1 waves in response to Arctic sea-ice loss, particularly over the Barents–Kara seas (BKS). Increased snow cover over the Eurasian continent may also have contributed to the shift. Our analysis reveals that the vortex shift induces cooling over some parts of the Eurasian continent and North America which partly offsets the tropospheric climate warming there in the past three decades. The potential vortex shift in response to persistent sea-ice loss in the future6,7, and its associated climatic impact, deserve attention to better constrain future climate changes.

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Figure 1: Polar vortex position and fractional area of regions covered by the polar vortex.
Figure 2: Polar vortex shifts associated with the sea-ice loss.
Figure 3: Analysis of meteorological fields.
Figure 4: Impact of the polar vortex shift.

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Acknowledgements

This work is supported by the National Science Foundation of China (41225018, 41575038). This work is also supported by the Foundation for Innovative Research Groups of the National Science Foundation of China (Grant No. 41521004). We thank S.-W. Son for comments and suggestions. Matlab codes for the linearized barotropic vorticity equation model support provided by J. Shaman and E. Tziperman are highly appreciated. We thank the scientific teams for ECMWF, NASA, Hadley Centre, CM SAF data and CMIP5 multi-model data. We also thank NCAR for providing the WACCM3 model.

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Authors and Affiliations

  1. Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000, China

    Jiankai Zhang, Wenshou Tian & Jinlong Huang

  2. School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK

    Martyn P. Chipperfield

  3. College of Global Change and Earth System Science, Beijing Normal University, Beijing 100875, China

    Fei Xie

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  1. Jiankai Zhang
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Contributions

J.Z. and W.T. contributed to writing the paper, design of the numerical experiments and data analysis. M.P.C. contributed to the discussion and writing the paper. F.X. contributed to the discussion and design of the numerical experiments. J.H. contributed to the data analysis. All authors reviewed the manuscript.

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Correspondence to Wenshou Tian.

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Zhang, J., Tian, W., Chipperfield, M. et al. Persistent shift of the Arctic polar vortex towards the Eurasian continent in recent decades. Nature Clim Change 6, 1094–1099 (2016). https://doi.org/10.1038/nclimate3136

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