Skip to main content

Thank you for visiting nature.com. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in Internet Explorer). In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript.

  • Article
  • Published:

Probability of US heat waves affected by a subseasonal planetary wave pattern

This article has been updated

Abstract

Heat waves are thought to result from subseasonal atmospheric variability. Atmospheric phenomena driven by tropical convection, such as the Asian monsoon, have been considered potential sources of predictability on subseasonal timescales. Mid-latitude atmospheric dynamics have been considered too chaotic to allow significant prediction skill of lead times beyond the typical 10-day range of weather forecasts. Here we use a 12,000-year integration of an atmospheric general circulation model to identify a pattern of subseasonal atmospheric variability that can help improve forecast skill for heat waves in the United States. We find that heat waves tend to be preceded by 15–20 days by a pattern of anomalous atmospheric planetary waves with a wavenumber of 5. This circulation pattern can arise as a result of internal atmospheric dynamics and is not necessarily linked to tropical heating. We conclude that some mid-latitude circulation anomalies that increase the probability of heat waves are predictable beyond the typical weather forecast range.

This is a preview of subscription content, access via your institution

Access options

Buy this article

Prices may be subject to local taxes which are calculated during checkout

Figure 1: Comparison of the model heat wave statistics with observations.
Figure 2: Temporal evolution of the heat waves.
Figure 3: Prominent subseasonal variability patterns.
Figure 4: Probability of the heat waves in CAM3 conditioned on the standardized amplitude of the wavenumber-5 pattern 15 days earlier (red bars).

Similar content being viewed by others

Change history

  • 30 October 2013

    In the version of this Article originally published online, the NOAA CPO's MAPP program was missing from the Acknowledgements. This has been corrected in all versions of the Article.

References

  1. Easterling, D. R. et al. Climate extremes: Observations, modelling, and impacts. Science 289, 2068–2074 (2000).

    Article  Google Scholar 

  2. Ebi, K. & Meehl, G. A. Heatwaves and Global Climate Change, The Heat is On: Climate Change and Heatwaves in the Midwest. Regional Impacts of Climate Change: Four Case Studies in the United States 8–21 (Pew Center on Global Climate Change, 2007).

    Google Scholar 

  3. Meehl, G. A. & Tebaldi, C. More intense, more frequent, and longer lasting heat waves in the 21st century. Science 305, 994–997 (2004).

    Article  Google Scholar 

  4. Madden, R. A. & Julian, P. R. Detection of a 40–50 day oscillation in the zonal wind in the tropical Pacific. J. Atmos. Sci. 28, 702–708 (1971).

    Article  Google Scholar 

  5. Waliser, D. E., Lau, K. M., Stern, W. & Jones, C. Potential predictability of the Madden–Julian oscillation. Bull. Am. Meteorol. Soc. 84, 33–50 (2003).

    Article  Google Scholar 

  6. Branstator, G., Mai, A. & Baumhefner, D. Identification of highly predictable flow elements for spatial filtering of medium- and extended-range numerical forecasts. Mon. Weath. Rev. 121, 1786–1802 (1993).

    Article  Google Scholar 

  7. DelSole, T. & Tippett, M. K. Predictable components and singular vectors. J. Atmos. Sci. 65, 1666–1678 (2008).

    Article  Google Scholar 

  8. Schubert, S., Wang, H. & Suarez, M. Warm seasonal subseasonal variability and climate extremes in the Northern Hemisphere: the role of stationary Rossby waves. J. Clim. 24, 4773–4792 (2011).

    Article  Google Scholar 

  9. Chen, P. & Newman, M. Rossby wave propagation and the rapid development of upper-level anomalous anticyclones during the 1988 US drought. J. Clim. 11, 2491–2504 (1998).

    Article  Google Scholar 

  10. Lyon, B. & Dole, R. M. A diagnostic comparison of the 1980 and 1988 US summer heat wave-droughts. J. Clim. 8, 1658–1675 (1995).

    Article  Google Scholar 

  11. Kalnay, E. et al. The NCEP/NCAR 40-year reanalysis project. Bull. Am. Meteorol. Soc. 77, 437–471 (1996).

    Article  Google Scholar 

  12. Branstator, G. Horizontal energy propagation in a barotropic atmosphere with meridional and zonal structure. J. Atmos. Sci. 40, 1689–1708 (1983).

    Article  Google Scholar 

  13. Hoskins, B. J. & Ambrizzi, T. Rossby wave propagation on a realistic longitudinally varying flow. J. Atmos. Sci. 50, 1661–1671 (1993).

    Article  Google Scholar 

  14. Namias, J. Anatomy of Great Plains protracted heat waves (especially the 1980 US summer drought). Mon. Weath. Rev. 110, 824–838 (1982).

    Article  Google Scholar 

  15. Chang, F.-C. & Wallace, J. M. Meteorological conditions during heat waves and droughts in the United States Great Plains. Mon. Weath. Rev. 115, 1253–1269 (1987).

    Article  Google Scholar 

  16. Plumb, R. A. On the three-dimensional propagation of stationary waves. J. Atmos. Sci. 42, 217–229 (1985).

    Article  Google Scholar 

  17. Karoly, D. J., Plumb, R. A. & Ting, M. Example of the horizontal propagation of quasi-stationary waves. J. Atmos. Sci. 46, 2802–2811 (1989).

    Article  Google Scholar 

  18. Hoskins, B. & Karoly, D. J. The steady linear response of a spherical atmosphere to thermal and orographic forcing. J. Atmos. Sci. 38, 1179–1196 (1981).

    Article  Google Scholar 

  19. Branstator, G. Organization of storm track anomalies by recurring low-frequency circulation anomalies. J. Atmos. Sci. 52, 207–226 (1995).

    Article  Google Scholar 

  20. Branstator, G. Circumglobal teleconnections, the jet stream waveguide, and the North Atlantic Oscillation. J. Clim. 15, 1893–1910 (2002).

    Article  Google Scholar 

  21. Ding, Q. & Wang, B. Circumglobal teleconnection in the Northern Hemisphere summer. J. Clim. 18, 3483–3505 (2005).

    Article  Google Scholar 

  22. Ding, Q., Wang, B., Wallace, J. M. & Branstator, G. Tropical-extratropical teleconnections in boreal summer: Observed interannual variability. J. Clim. 24, 1878–1896 (2011).

    Article  Google Scholar 

  23. Newman, M. & Sardeshmukh, P. D. The impact of the annual cycle on the North Pacific/North American response to remote low-frequency forcing. J. Atmos. Sci. 55, 1336–1353 (1998).

    Article  Google Scholar 

  24. Erich, E. et al. Soil moisture-atmosphere interactions during the 2003 European summer heat wave. J. Clim. 20, 5081–5099 (2007).

    Article  Google Scholar 

  25. Collins, W. D. et al. The Community Climate System Model version 3 (CCSM3). J. Clim. 19, 2122–2143 (2006).

    Article  Google Scholar 

  26. Gent, P. et al. The community climate system model version 4. J. Clim. 24, 4973–4991 (2011).

    Article  Google Scholar 

Download references

Acknowledgements

We thank A. Mai for carrying out the experiment and S. Schubert for comments. Portions of this study were supported by the Office of Science (BER), US Department of Energy, NASA NEWS, NOAA CPO's MAPP program and the National Science Foundation. NCAR is sponsored by the National Science Foundation. Computing resources were provided by NCAR’s Computational and Information Systems Laboratory and by the National Energy Research Scientific Computing Center, which is supported by BER of the US Department of Energy.

Author information

Authors and Affiliations

Authors

Contributions

H.T. and G.B. led the analysis and all authors contributed to writing of the paper.

Corresponding author

Correspondence to Haiyan Teng.

Ethics declarations

Competing interests

The authors declare no competing financial interests.

Supplementary information

Supplementary Information

Supplementary Information (PDF 3101 kb)

Rights and permissions

Reprints and permissions

About this article

Cite this article

Teng, H., Branstator, G., Wang, H. et al. Probability of US heat waves affected by a subseasonal planetary wave pattern. Nature Geosci 6, 1056–1061 (2013). https://doi.org/10.1038/ngeo1988

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1038/ngeo1988

This article is cited by

Search

Quick links

Nature Briefing

Sign up for the Nature Briefing newsletter — what matters in science, free to your inbox daily.

Get the most important science stories of the day, free in your inbox. Sign up for Nature Briefing