Extreme weather in a changing climate

First published 19 September 2023, in Environmental Research Letters 18; reproduced here under Creative Commons Attribution 4.0 licence

Authors:

1. Giorgia Di Capua:Magdeburg-Stendal University of Applied Sciences, 39114 Magdeburg, Germany

2. Stefan Rahmstorf: Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, PO Box 6012 03, D-14412 Potsdam, Germany | E-mail: [email protected]
   
   

Abstract

Extreme weather events are rising at a pace which exceeds expectations based on thermodynamic arguments only, changing the way we perceive our climate system and climate change issues. Every year, heatwaves, floods and wildfires, bring death and devastation worldwide, increasing the evidence about the role of anthropogenic climate change in the increase of extremes. In this viewpoint article, we summarize some of the most recent extremes and put them in the context of the most recent research on atmospheric and climate sciences, especially focusing on changes in thermodynamics and dynamics of the atmosphere. While some changes in extremes are to be expected and are clearly attributable to rising greenhouse gas emissions, other seem counterintuitive, highlighting the need for further research in the field. In this context, research on changes in atmospheric dynamics plays a crucial role in explaining some of these extremes and more needs to be done to improve our understanding of the physical mechanisms involved.

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A rise in weather extremes is probably the most severe early impact of rising global temperatures. Extreme weather events have a high impact on both human activities and natural ecosystems. In recent decades the world has seen an increase in heatwaves, droughts, flooding events and fire weather conditions, as expected in a warming climate. 2022 has been no exception, with record-breaking high temperatures registered across large portions of Western Europe, China and Pakistan (Hausfather 2023). In Pakistan, extreme monsoon rains and Himalayan glaciers melting away in a heat wave have flooded approximately 85 000 km2 (USAID 2022), killing more than 1700 people and causing $15 billion of damage (World Bank), while the Horn of Africa has seen an unprecedented drought that has pushed more than three million people into emergency food insecurity (NASA Earth Observatory 2022). Many of these events have been made more likely by anthropogenic warming and represent a serious threat to human society, with effects ranging from health and mortal- ity to economy and national security issues.

Even for lay persons it will be obvious that heat extremes will increase in a warming world. But it may be unexpected by how much: monthly heat extremes

that were three standard deviations above average during the baseline period 1951–1980 have already increased over 90-fold in frequency over the global land area, while the formerly near-unprecedented 4-sigma events have increased 1000-fold to affect 3% of the land area in any given month, data show (Robinson et al 2021). July 2023 was the hot- test month on record on Earth by a large margin (Copernicus 2023a), and likely the hottest for at least 10 000 years. Marine heatwaves have also doubled in the last few decades, and they are expected to see a 23-fold increase under a 2 ◦C warming scenario (Frölicher et al 2018)—the off-the charts sea surface temperatures in the North Atlantic in summer 2023 are a stern foretaste of this (Copernicus 2023b), while in Florida the marine heatwave caused wide spread bleaching turning into one of the worst events in the region on record (Dennis et al 2023).

Part of this is as expected simply by shifting a Gaussian normal distribution towards warmer values; the more extreme an event, the larger is the factor by which its likelihood increases. However, explaining the full extent of the global increase in extreme heat requires additional, dynamical effects (which we will discuss below).

And heat—especially lasting heat—is a silent killer. The death toll of the 2003 European heat wave has been estimated as ∼70 000 (Robine et al 2008), with a mortality peak in France higher than dur- ing any Covid19 wave (Ferrer and Breteau 2020). A first estimate for summer 2022 came in at ∼62 000 (Ballester et al 2023), when even in Britain temperatures soared above 40◦C for the first time in history. Temperature-related excess mortality is expected to increase with unmitigated global warming, even when accounting for a decrease in cold-related deaths (Gasparrini et al 2017).

Since early 2012, the fingerprint of climate change can be detected in any single day in the observed record. There are no more days on Earth where global weather is not significantly different from what it would be without human influence—on nearly all days even when just considering the weather pat- terns without the increase in global-mean temperature (Sippel et al 2020). Observations show that nearly the entire Earth surface has warmed since the late 19th century (except for the prominent ‘warming hole’ south of Greenland and Iceland, Rahmstorf et al 2015) and the annual global mean temperature has increased by 1.2◦C since the late 19th Century (Intergovernmental Panel on Climate Change 2021). The intensity and speed of warming differ by region, with land areas warming twice as much as the ocean surface since 1970 (Intergovernmental Panel on Climate Change 2021). Warming is more prominent in the Arctic, Eastern Europe, North Africa, the Middle East, East Asia and western North America. Key heatwave characteristics, such as frequency, duration and cumulative heat (i.e. the heat produced by heatwaves days inside a season), show increasing trends since 1950 at global scale, with stronger trends in tropical and northern latitudes. Trends for these key variables have been accelerating in the past few decades (Perkins-Kirkpatrick and Lewis 2020). Summer 2023 was no exception, with record breaking temperature recorded in Southeastern US, China, Spain, Morocco, rendered more likely by current climate change (Zachariah et al 2023).

While the world-wide rise in heat extremes is easily understood given the rise in global mean temperature, mean global rainfall and extreme precipitation trends depict a more complex relationship. Global rainfall is expected to increase as evaporation from warmer oceans increases. Indeed, the IPCC AR6 WGI (2021) reports an increase in globally averaged land precipitation since 1950, though with medium confidence given the large variability and spatial heterogeneity of precipitation. However, extreme rainfall events have shown a steep increase in the last few decades (especially in tropical regions), with 1 in 4 record breaking rainfall events being attributable to climate change (Robinson et al 2021). In August 2023, the region surrounding Beijing was hit by a severe flood event which saw the highest rainfall record of

the last 140 years (744.8 mm in less the 4 d) (Hawkins 2023) Perhaps counterintuitively, some areas even show opposite trends in mean precipitation rates and extreme rainfall events. One such example is the Indian summer monsoon system, which shows a slight decrease in its mean seasonal precipitation rates together with a three-fold increase in extreme rainfall events during the 1950–2015 period (Roxy et al 2017). Therefore, when considering the effect of climate change on extremes, it is not enough to look at trends in mean values.

Another example of that is that despite the global-mean (and often also local) rainfall increase, the frequency and severity of droughts has also increased in some regions, for a number of reasons. One overall reason is that with approximately constant relative humidity, air will contain (and at some point rain out) 7% more moisture per degree of warming, while the resupply of water via evaporation increases only by 2%–3% per degree (Allan et al 2020). The additional evaporation and rain- fall tends to end up in heavy rain rather than alleviating drought: Half of it comes down in the wet- test 6 d each year (Pendergrass and Knutti 2018), and the heaviest rainfall events increase most strongly (Fischer and Knutti 2015). Also, increasing agricultural and ecological droughts (i.e. loss of soil moisture and drying vegetation) can be caused not just by declining precipitation but also by rising temperatures causing faster evapotranspiration. In different regions, either of these effects can be the more important one (Cook et al 2018). Major droughts can also result from natural climate variability and are rare events (compared to the length of available observational data). Thus, studying their trend and, more importantly, attributing them to anthropogenic global warming is not an easy task (Cook et al 2018). Several regions in the world have shown an increase in drought risk, such as Western North America, the Mediterranean, East Southern Africa, East Asia and South Australia, at least partly attributable to anthropogenic warming, with the Mediterranean and the North-Western North America showing the highest confidence (Intergovernmental Panel on Climate Change 2021).

In the past decade, wildfire activity has produced some new extreme fires that are unprecedented regarding propagation speed, intensity, location, timing and burnt area (Descals et al 2022, Senande- Rivera et al 2022). For example, the Australian ‘Black Summer’ wildfire disaster in 2019/2020 fol- lowed Australia’s hottest and driest year on record, burned more than half of the habitat for over 1600 native species and directly caused 33 human deaths and almost 450 more from smoke inhalation (Himbrechts 2021). An increase in extreme fire weather conditions can already be detected at global scale, although trend magnitude and spatial patterns vary at regional scale (Jain et al 2022). Globally, anthropogenic global warming is projected to cause unprecedented increases in extreme fire weather risk in the 21st century (Touma et al 2021). Model experiments estimate that anthropogenic induced changes in fire weather indices have already emerged from natural variability for 22% of the burnable land area globally by 2019, while by the mid twenty-first century the emergence will reach 30%–60% (Abatzoglou et al 2019). Meanwhile, in August 2023, Hawaii has experienced its worst wildfire on record, and one of the worst in US history, where dry conditions and hurricane-force winds fueled the flames bringing utter devastation to the town of Lahaina, killing at least 93 people and thus surpassing the death toll of the Camp fire in California in 2018 (Gabbat and Anguiano 2023).

While warm extremes are to be expected due to anthropogenic global warming, cold extreme are projected to decrease in this century. Nevertheless, despite the general increase in global surface temperatures, a few regions show a cooling trend in the historical record. One such example is central Siberia, which features a cooling trend during boreal winter (Inoue et al 2012). While both natural variability and anthropogenic forcing are debated as causes of this trend (Inoue et al 2012), the cooling trend is mainly associated with an increase in cold extremes over the region. Cold air outbreaks in central Siberia and North America have been shown to result from sudden stratospheric warming events and a disruption of the stratospheric Polar vortex (Kretschmer et al 2018).

Detecting climate change signals can be challenging depending on the region and the variable selected, and attributing trends in temperature or precipitation fields to changes in thermodynamic or dynamic features of the atmosphere represent an even greater challenge (Shepherd 2014). In general, the largest portion of the change is to be attributed to thermodynamic effects. However, dynamic changes can further exacerbate thermodynamic driven changes and atmosphere dynamics and changes in weather patterns play an important role at regional scale (Rousi et al 2022). Amplified Rossby waves with preferred phase position, in particular waves with wave numbers 5 and 7, can lead to concurrent heatwaves (and crop failures) in the mid-latitudes (Kornhuber et al 2020), raising concerns about future food security. Arctic amplification, despite being more prominent in winter than summer, may also affect westerly winds, storm tracks and wave-guides in the mid-latitudes (Coumou et al 2018). Analyzing the ability of models to reproduce amplified waves 5 and 7 shows that even a small bias in upper tropospheric circulation features can have a strong impact on surface temperature and rainfall patterns (Luo et al 2022), highlighting that it is difficult for global climate models to simulate all mechanisms that contribute to making weather more extreme.

Europe has emerged as a hot-spot of heat extremes: it has seen a stronger increase in summer heat than other regions in the northern mid-latitudes. This enhanced warming has been related to dynamical changes such as an increase of double jet patterns, which could explain all of the additional rise in heat waves beyond what is expected simply by thermodynamics (Rousi et al 2022). Both observation and model experiment support the hypothesis that shrinking Arctic sea ice and reduced snow cover over northern Eurasia in spring can also contribute to increased blocking over Europe and consequent frequency of heatwaves (Zhang et al 2020). Sea surface temperature anomalies (in particular the northern Atlantic ‘warming hole’ mentioned earlier) can also reinforce heatwaves in central Europe, such as in 2015 (Duchez et al 2015).

In summary, it is now clear that global warming is already greatly increasing the number and intensity of many types of weather extremes, as has been predicted by climate science for decades. Much of this is due to thermodynamics. With that we mean that the atmosphere is warmer, which means it holds more energy and water to power extreme weather. The ocean is also warmer and can provide more energy and moisture as fuel to tropical cyclones. However, increasingly the attention of researchers has turned to dynamic effects. With that we refer to changes in circulation and stability of atmosphere and ocean. It includes changes to the jet stream, polar vortex, atmospheric planetary waves or to the Atlantic meridional overturning circulation.

Obtaining robust conclusions about changes in weather extremes requires long time series, given that extreme events are by definition rare events and are not easy to model. Nevertheless, the signal of climate change has now clearly emerged from the noise for many types of extremes. Disentangling the dynamic mechanisms is harder again and represents a current frontline of research. Driving forces behind dynamic changes are often regionally diverse temperature changes, such as Arctic amplification, enhanced land warming and sea surface temperature anomalies. Many facets of the dynamic mechanisms are still being debated in the scientific literature. Even if not everything is fully understood, researchers and journalists should not be shy to use every opportunity to educate the public about the fact that human-caused global warming is making weather extremes worse, already causing serious harm to many millions of people.

Even once global warming is stopped, we will see unprecedented extremes for a long time to come. Just think of a former once-in-5000 year event which at 1.5◦C warming may have become a once-in-50 year event. Thus, it will take many decades until we have seen all the possible extreme events a 1.5◦C warmer world has in store for us.

References

Abatzoglou J T, Williams A P and Barbero R 2019 Global emergence of anthropogenic climate change in fire weather indices Geophys. Res. Lett. 46 326–36

Allan R P et al 2020 Advances in understanding large-scale responses of the water cycle to climate change Ann. New York Acad. Sci. 1472 49–75

Ballester J, Quijal-zamorano M, Fernando R, Turrubiates M, Pegenaute F, Herrmann F R, Robine J M and Basagan ̃a X 2023 Heat-related mortality in Europe during the summer of 2022 Nat. Med. 29 1857–66

Cook B I, Mankin J S and Anchukaitis K J 2018 Climate change and drought: from past to future Curr. Clim. Change Rep. 4 164–79

Copernicus 2023a July 2023 sees multiple global temperature records broken Copernicus (available at: https://climate. copernicus.eu/july-2023-sees-multiple-global-temperature- records-broken)

Copernicus 2023b Record-breaking North Atlantic Ocean temperatures contribute to extreme marine heatwaves Copernicus Online (available at: https://climate.copernicus. eu/record-breaking-north-atlantic-ocean-temperatures- contribute-extreme-marine-heatwaves)

Coumou D, Di Capua G, Vavrus S, Wang L and Wang S 2018 The influence of Arctic amplification on mid-latitude summer circulation Nat. Commun. 9 2959

Dennis B, Ajasa A and Mooney C 2023 As Florida ocean temperatures soar, a race to salvage imperiled corals (Washington Post) (available at: www.washingtonpost.com/ climate-environment/2023/07/26/florida-coral-reef-ocean- temperatures-heat/)

Descals A, Gaveau D L A, Verger A, Sheil D, Naito D and Pen ̃uelas J 2022 Unprecedented fire activity above the Arctic circle linked to rising temperatures Science 378 532–7

Duchez A, Frajka-williams E, Josey S A, Evans D G, Grist J P, Marsh R, McCarthy G D, Sinha B, Berry D I and Hirschi J J-M 2015 Drivers of exceptionally cold North Atlantic Ocean temperatures and their link to the 2015 European heat wave Environ. Res. Lett. 11 1–9

Ferrer M and Breteau P 2020 Coronavirus: un pic très net de mortalité en France enregistré en mars et avril Le Monde (available at: www.lemonde.fr/les-decodeurs/article/2020/ 04/27/coronavirus-un-pic-tres-net-de-mortalite-en-france- depuis-le-1er-mars-par-rapport-aux-vingt-dernieres- annees_6037912_4355770.html)

Fischer E M and Knutti R 2015 Anthropogenic contribution to global occurrence of heavy-precipitation and high-temperature extremes Nat. Clim. Change 5 560–4

Frölicher T L, Fischer E M and Gruber N 2018 Marine heatwaves under global warming Nature 560 360–4

Gabbat A and Anguiano D 2023 Hawaii wildfires: deadliest US blaze in a century kills at least 93 people Guard (available at: www.theguardian.com/us-news/2023/aug/13/hawaii- wildfires-at-least-89-confirmed-killed-after-deadliest-us- blaze-in-100-years)

Gasparrini A et al 2017 Projections of temperature-related excess mortality under climate change scenarios Lancet Planet. Health 1 e360–7

Hausfather Z 2023 State of the climate: how the world warmed in 2022 Carbon Brief (available at: www.carbonbrief.org/state- of-the-climate-how-the-world-warmed-in-2022/)

Hawkins A 2023 Chinese firefighter ‘dies heroic death’ as Beijing reports heaviest rain in 140 years Guard (available at: www. theguardian.com/world/2023/aug/02/beijing-reports- heaviest-rain-140-years-china-g20-climate-talks)

Himbrechts D 2021 Australia’s Black Summer of fire was not normal—and we can prove it The Conversation (available at: https://theconversation.com/australias-black-summer-of- fire-was-not-normal-and-we-can-prove-it-172506)

Inoue J, Hori M E and Takaya K 2012 The role of Barents Sea ice in the wintertime cyclone track and emergenceof a warm-Arctic cold-Siberian anomaly J. Clim. 25 2561–9

IPCC 2021 Climate Change 2021: The Physical Science Basis.

Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change ed V Masson-Delmotte et al (Cambridge University Press) (https://doi.org/10.1017/9781009157896)

Jain P, Castellanos-Acuna D and Coogan S C P 2022 Observed increases in extreme fire weather driven by atmospheric humidity and temperature Nat. Clim. Chang. 12 63–70

Kornhuber K, Coumou D, Vogel E, Lesk C, Donges J F, Lehmann J and Horton R M 2020 Amplified Rossby waves enhance risk of concurrent heatwaves in major breadbasket regions Nat. Clim. Change 20 48–53

Kretschmer M, Cohen J, Matthias V, Runge J and Coumou D 2018 The different stratospheric influence on cold-extremes in Eurasia and North America npj Clim. Atmos. Sci. 1 1–10

Luo F et al 2022 Summertime Rossby waves in climate models: substantial biases in surface imprint associated with small biases in upper-level circulation Weather Clim. Dyn.
3 905–35

NASA Earth Observatory 2022 Worst Drought on Record Parches Horn of Africa (available at: https://earthobservatory.nasa. gov/images/150712/worst-drought-on-reco)

Pendergrass A G and Knutti R 2018 The uneven nature of daily precipitation and its change Geophys. Res. Lett.
45 980–11,988

Perkins-Kirkpatrick S E and Lewis S C 2020 Increasing trends in regional heatwaves Nat. Commun. 11 1–8

Rahmstorf S, Box J E, Feulner G, Mann M E, Robinson A, Rutherford S, Scha E J and Schaffernicht E J 2015 Exceptional twentieth-century slowdown in Atlantic Ocean overturning circulation Nat. Clim. Change 5 475–80

Robine J M, Cheung S L K, Le Roy S, Van Oyen H, Griffiths C, Michel J P and Herrmann F R 2008 Death toll exceeded 70,000 in Europe during the summer of 2003 C. R. Biol. 331 171–8

Robinson A, Lehmann J, Barriopedro D, Rahmstorf S and Coumou D 2021 Increasing heat and rainfall extremes now far outside the historical climate npj Clim. Atmos. Sci. 4 3–6

Rousi E, Kornhuber K, Beobide-Arsuaga G, Luo F and Coumou D 2022 Accelerated western European heatwave trends linked to more-persistent double jets over Eurasia Nat. Commun. 13 1–11

Roxy M K, Ghosh S, Pathak A, Athulya R, Mujumdar M, Murtugudde R, Terray P and Rajeevan M 2017 A threefold rise in widespread extreme rain events over central India Nat. Commun. 8 1–11

Senande-Rivera M, Insua-Costa D and Miguez-Macho G 2022 Spatial and temporal expansion of global wildland fire activity in response to climate change Nat. Commun.
13 1–9

Shepherd T G 2014 Atmospheric circulation as a source of uncertainty in climate change projections Nat. Geosci. 7 703–8

Sippel S, Meinshausen N, Fischer E M, Székely E and Knutti R 2020 Climate change now detectable from any single day of weather at global scale Nat. Clim. Change 10 35–41

Touma D, Stevenson S, Lehner F and Coats S 2021 Human-driven greenhouse gas and aerosol emissions cause distinct regional impacts on extreme fire weather Nat. Commun. 12 1–8

USAID 2022 Pakistan Flood Fact Sheet (available at: www.usaid. gov/sites/default/files/2022-12/2022-09- 30_USG_Pakistan_Floods_Fact_Sheet_8.pdf)

Zachariah M, Philip S, Pinto I, Vahlberg M, Singh R, Arrighi J R, Barne C and Otto F E L 2023 Extreme heat in North America, Europe and China in July 2023 made much more likely by climate change (https://doi.org/10.25561/105549)

Zhang R, Sun C, Zhu J, Zhang R and Li W 2020 Increased European heat waves in recent decades in response to shrinking Arctic sea ice and Eurasian snow cover npj Clim. Atmos. Sci. 3 7