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Will there be more heatwaves in the future?

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As the climate becomes warmer, heatwaves become more likely. This is a trend that can already be observed, and that will continue in the future.

Illustration showing that heatwaves will become more common in a changing climate.

Heatwaves will become increasingly common in a changed climate.

In Scandinavia, a heatwave that currently occurs every twenty years might become so common that it occurs every five years. In southern Europe, heatwaves might become even more frequent. The change is thus different in different parts of the world.

Nor is the change in heatwaves proportional to the change in average temperatures. On a global scale, heatwaves are expected to double in frequency if the global average temperature rises by half a degree. Seemingly small limitations on the global temperature have a large effect on the frequency of heatwaves.

Heatwaves in a changed climate

It is hard to link individual weather events to climate change. Heatwaves occur when high pressure blocks – part of the weather’s random variations – build up.

However, the likelihood of heatwaves is increasing and the same weather conditions result in higher temperatures today than they did fifty years ago. These methods make it possible to demonstrate that some of the heatwaves in recent years probably would not have happened or would have been less extreme had it not been for global warming.

Research project

The information on this page is gathered in the Heatwaves subproject within the HazardSupport research project (2015-2020).

HazardSupport

References

Yan, Z., Jones, PD., Davies, T.D., Moberg, A., Bergström, H., Camuffo, D., Cocheo, C., Maugeri, M., Demarée, GR, Verhoeve, T., Thoen, E., Barriendos, M., Rodgríguez, R., Martiín-Vide, J., Yang, C., 2002: Trend of extreme temperatures in Europe and China based on daily observations. Climatic Change 53: 355–392. doi.org/10.1023/A:1014939413284 External link.

Della-Marta, P.M., J. Luterbacher, H. von Weissenfluh, E. Xoplaki, M. Brunet, and H. Wanner, 2007: Summer heat waves over western Europe 1880-2003, their relationship to large-scale forcings and predictability. Climate Dynamics, 29(2-3), 251-275. doi.org/10.1007/s00382-007-0233-1 External link.

Nikulin, G., E. Kjellström, U. Hansson, G. Strandberg, and A. Ullerstig, 2011: Evaluation and future projections of temperature, precipitation and wind extremes over Europe in an ensemble of regional climate simulations. Tellus A, 63, 41–55. doi.org/10.1111/j.1600-0870.2010.00466.x External link.

Collins, M., R. Knutti, J. Arblaster, J.-L. Dufresne, T. Fichefet, P. Friedlingstein, X. Gao, W.J. Gutowski, T. Johns, G. Krinner, M. Shongwe, C. Tebaldi, A.J. Weaver and M. Wehner, 2013: Long-term Climate Change: Projections, Commitments and Irreversibility. In: Climate Change 2013: The Physical Science Basis External link.. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)].

Dosio A et al 2018: Extreme heat waves under 1.5 °C and 2 °C global warming Environ. Res. Lett. 13 05400. doi.org/10.1088/1748-9326/aab827 External link.

Otto, F. E. L., N. Massey, G. J. van Oldenborgh, R. G. Jones, and M. R. Allen (2012), Reconciling two approaches to attribution of the 2010 Russian heat wave, Geophys. Res. Lett., 39, L04702, doi:10.1029/2011GL050422 External link.

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