Skip to main content
Log in

Atmospheric response to the South Pacific Subtropical Dipole

  • Published:
Climate Dynamics Aims and scope Submit manuscript

Abstract

Recent studies have suggested a dipolar mode of sea surface temperature variability in the subtropical South Pacific that matures in the austral summer, which is known as the South Pacific Subtropical Dipole (SPSD). In our study, the summer atmospheric response to the SPSD is investigated using observational data and numerical model experiments. Our results show a baroclinic response equatorward of 30° S and a barotropic response poleward of 30° S. The SPSD causes precipitation anomalies over the subtropical South Pacific, and the associated diabatic heating induces a baroclinic response. The mid- and high-latitude barotropic response is similar to the Southern Annual Mode (SAM) and is accompanied by an anomalous shift of storm tracks. The associated anomalous eddy activity is responsible for the SAM-like response. The results of numerical model experiments are consistent with our observations, except for the weak response in the high latitude. In the subtropical South Pacific, the spatial pattern of atmospheric response to the SPSD resembles the atmospheric anomalies that force the SPSD. The subtropical atmospheric response and the SPSD interact with each other and comprise a coupled system.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11
Fig. 12
Fig. 13

Similar content being viewed by others

References

Download references

Acknowledgements

We thank the anonymous reviewers for their constructive comments. This work was supported by the Natural Science Foundation of China (41606018, 41776035), Funds for Creative Research Groups of China (41421005). The observation datasets (ERSSTv5, NCEP/NCAR reanalysis, and CMAP precipitation) were downloaded from PSL/NOAA (https://psl.noaa.gov/data/gridded/). The CESM code is provided from NCAR and the experiments were performed in the High Performance Computing Center of Institute of Oceanology of CAS. Data processing and graphing work were finished using the NCAR Command Language (https://doi.org/10.5065/D6WD3XH5).

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Jian Zheng.

Additional information

Publisher's Note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Zheng, J., Wang, F. Atmospheric response to the South Pacific Subtropical Dipole. Clim Dyn 56, 1753–1765 (2021). https://doi.org/10.1007/s00382-020-05559-x

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00382-020-05559-x

Keywords

Navigation