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Flash floods and Urban flooding

Vulnerabilities - Global trends in flood mortality

Over the last five decades, floods have become less deadly. The global number of flood events has increased over time, but the average number of people killed and affected per event has decreased. This was concluded from an analysis of global data of flood fatalities for the period 1975–2022 (24). These data are part of the widely used EM-DAT International Disaster Database (https://www.emdat.be). The analysis includes 5582 flood events with one or more fatalities.


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Vulnerabilities - flash floods due daily rainfall extremes

Flash floods caused on average 50 casualties per year in Europe, 70% of the total number of deaths due to floods (8). The fatalities mainly occur in countries surrounding the Mediterranean Sea, where large population density exists at the coastal areas due to the important urbanization processes in this area during the last decades (9). Particularly in Spain, almost 90% of the victims due to floods are caused by flash floods (10). 

Changes in river flow extremes at a +2°C global warming are currently of central interest as this is the global target defined by policymakers to lower international greenhouse gases emissions. The impacts of a +2°C global warming on extreme floods (due to daily rainfall extremes) have been assessed for Europe for 1 in 10 and 1 in 100 year events. This was done for a combination of different models (global and regional climate models, hydrological models); the changes in floods were compared with the reference period 1971 - 2000 (2).

For floods (due to daily rainfall extremes) the results indicate a clear North to South gradient in future changes in flood magnitude:

  • South the 60°N line: a strong increase in flood magnitudes, due to changes in extreme rainfall, except for some regions in Bulgaria, Czech Republic, Poland, the western Balkans, the Baltic countries, and southern Spain where no significant changes can be detected. Floods are even increasing in areas such as southern Mediterranean where the average discharge is projected to decrease (3).
  • Above the 60°N line: a relatively strong decrease in flood magnitude in parts of Finland, NW Russia and North of Sweden with the exception of southern Sweden and some coastal areas in Norway where increases in floods are projected. Projections of decreasing flood magnitudes are mainly due to the decreases in snowpack in areas where most of the floods are caused by spring snowmelt in combination with rainfall. Increases in flood magnitude in Scandinavia are mainly seen in coastal areas where the rain-fed floods will increase (2). 

Intense rainstorms are moving more slowly, causing more floods

Intense rainstorms can flood cities and produce deadly flash floods. In previous decades, these extreme precipitation events were quite common in especially southern Europe. In the summer of 2021, we’ve seen such an event over parts of Germany, Belgium and the Netherlands, causing more than 200 casualties and billions of Euros in damage. With global warming, these events are expected to occur more frequent throughout Europe for two reasons (23).

The first reason is an obvious one. Warmer air can hold more moisture, about 7% per degree of warming. That’s why these intense rainstorms are typically a summer phenomenon. The second reason may come as a surprise. Rainstorms are expected to move more slowly with global warming, exposing a certain area to the extreme precipitation of one event for a longer period. This slowing-down is linked to the difference in temperature between the poles and the tropics. This difference determines the strength of winds high in the atmosphere. A larger difference leads to stronger winds. But the poles are warming much faster than the tropics, and this difference is getting smaller. With slower winds, rainstorms move more slowly from one place to another (23).

Not all intense rainstorms are moving slowly. Only about 3 to 4% are slow-moving events. Changes in their frequency of occurrence are extremely important, however. These are the rainstorms that are most devastating because they can accumulate extremely large volumes of water in a small area, causing flooding (23).

By the end of the century, intense rainstorms may become 7 times more frequent in Europe, according to a recent study. The part of these storms that are moving slowly may become 14 times more frequent. This projection is based on a high-end scenario (RCP 8.5) that most scientist consider unrealistically high. The results do issue a warning, though: A future reduction in the speed of rainstorms could enhance the risk of flash flooding to a much higher level than one would expect from just the higher moist content of warmer air. The higher frequency of (slowly moving) intense rainstorms will affect all of Europe. Just like now, southern Europe will still experience the highest frequency of cases in the future (23).

Vulnerabilities - Urban drainage

An urban drainage system may damp or amplify changes in precipitation, depending on the system characteristics. The combined impact of climate change and increased urbanisation in some parts of the North Sea region could result in as much as a four-fold increase in sewer overflow volumes (6). For Roskilde (Denmark), for instance, a 40% increase in design rainfall intensities was found to increase the current level of damage costs related to sewer flooding by a factor of 10 (4). The actual change in cost will depend on catchment and sewer system characteristics. The impacts of climate change on sewer flood and overflow frequencies and volumes show wide variation. Studies indicate a range from a four-fold increase to as low as a 5 % increase, depending on the system characteristics (5).


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Adaptation strategies

At many places climate change both increases droughts and heavy rainfall. Too little and too much water are part of the same problem. They may be part of the same solution too: by redesigning the storm water infrastructure of cities.  

When it rains hard, the sudden volume of water can overwhelm urban drainage systems and lead to flash flooding. Slowing down this discharge and collecting part of it in reservoirs can overcome this. In fact, by storing it we can safe the water for the future, and we can turn troublesome storm water into a resource. Vegetation planted in and around the reservoir purifies the water because the pollutants become trapped in the soil or the roots, and contaminants are taken up by tissues or even broken down into less harmful substances. The cleaner water can then be further purified and allowed to percolate into underground aquifers beneath the city, where it can serve as a drinking-water source during droughts (1).


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References

The references below are cited in full in a separate map 'References'. Please click here if you are looking for the full references for Europe.

  1. Gaines (2016)
  2. Roudier et al. (2016)
  3. Greuell et al. (2015), in: Roudier et al. (2016)
  4. Arnbjerg-Nielsen and Fleischer (2009), in: Willems and Lloyd-Hughes (2016)
  5. Willems et al. (2012a, b), in: Willems and Lloyd-Hughes (2016)
  6. Willems and Lloyd-Hughes (2016)
  7. Olsson et al. (2010), in: Willems and Lloyd-Hughes (2016)
  8. Barredo (2007), in: Pino et al. (2016) 
  9. Llasat et al. (2010), in: Pino et al. (2016)
  10. Olcina and Ayala-Carcedo (2002), in: Pino et al. (2016)
  11. Moore et al. (2016)
  12. Gaffin et al. (2012), in: Moore et al. (2016)
  13. Heidrich et al. (2013), in: Moore et al. (2016)
  14. Ercolani et al. (2018)
  15. Berndtsson (2010); Chang et al. (2015); Soulis et al. (2017); Shafique et al. (2018), all in: Quaranta et al. (2021)
  16. Susca et al. (2011); La Roche and Berardi (2014), both in: Quaranta et al. (2021)
  17. Issa et al. (2015), in: Quaranta et al. (2021)
  18. Whittinghill et al. (2014); Kuronuma et al. (2018), both in: Quaranta et al. (2021)
  19. Colla et al. (2009); Fernández Cañero and González Redondo (2010), both in: Quaranta et al. (2021)
  20. Van Renthergem and Botteldooren (2009), in: Quaranta et al. (2021)
  21. Blackhurst et al. (2010); Orisini et al. (2014); Baldock et al. (2019), all in: Quaranta et al. (2021)
  22. Quaranta et al. (2021)
  23. Kahraman et al. (2021)
  24. Jonkman et al. (2024)

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