Showing posts with label Extreme Floods. Show all posts
Showing posts with label Extreme Floods. Show all posts

Mar 28, 2024

Land under water: What causes extreme flooding?

If rivers overflow their banks, the consequences can be devastating -- just like the catastrophic floods in North Rhine-Westphalia and Rhineland-Palatinate of 2021 showed. In order to limit flood damage and optimise flood risk assessment, we need to better understand what factors can lead to extreme forms of flooding and to what extent. Using methods of explainable machine learning, researchers at the Helmholtz Centre for Environmental Research (UFZ) have shown that floods are more extreme when several factors are involved in their development. The research was published in Science Advances.

There are several factors that play an important role in the development of floods: air temperature, soil moisture, snow depth, and the daily precipitation in the days before a flood. In order to better understand how individual factors contribute to flooding, UFZ researchers examined more than 3,500 river basins worldwide and analysed flood events between 1981 and 2020 for each of them. The result: precipitation was the sole determining factor in only around 25% of the almost 125,000 flood events. Soil moisture was the decisive factor in just over 10% of cases, and snow melt and air temperature were the sole factors in only around 3% of cases. In contrast, 51.6% of cases were caused by at least two factors. At around 23%, the combination of precipitation and soil moisture occurs most frequently.

However, when analysing the data, the UFZ researchers discovered that three -- or even all four -- factors can be jointly responsible for a flood event. For example, temperature, soil moisture, and snow depth were decisive factors in around 5,000 floods whilst all four factors were decisive in around 1,000 flood events. And not only that: "We also showed that flood events become more extreme when more factors are involved," says Dr Jakob Zscheischler, Head of the UFZ Department "Compound Environmental Risks" and senior author of the article. In the case of one-year floods, 51.6% can be attributed to several factors; in the case of five- and ten-year floods, 70.1% and 71.3% respectively can be attributed to several factors. The more extreme a flood is, the more driving factors there are and the more likely they are to interact in the event generation. This correlation often also applies to individual river basins and is referred to as flood complexity.

According to the researchers, river basins in the northern regions of Europe and America as well as in the Alpine region have a low flood complexity. This is because snow melt is the dominant factor for most floods regardless of the flood magnitude. The same applies to the Amazon basin, where the high soil moisture resulting from the rainy season is often a major cause of floods of varying severity. In Germany, the Havel and the Zusam, a tributary of the Danube in Bavaria, are river basins that have a low flood complexity. Regions with river basins that have a high flood complexity primarily include eastern Brazil, the Andes, eastern Australia, the Rocky Mountains up to the US west coast, and the western and central European plains. In Germany, this includes the Moselle and the upper reaches of the Elbe. "River basins in these regions generally have several flooding mechanisms," says Jakob Zscheischler. For example, river basins in the European plains can be affected by flooding caused by the combination of heavy precipitation, active snow melt, and high soil moisture.

However, the complexity of flood processes in a river basin also depends on the climate and land surface conditions in the respective river basin. This is because every river basin has its own special features. Among other things, the researchers looked at the climate moisture index, the soil texture, the forest cover, the size of the river basin, and the river gradient. "In drier regions, the mechanisms that lead to flooding tend to be more heterogeneous. For moderate floods, just a few days of heavy rainfall is usually enough. For extreme floods, it needs to rain longer on already moist soils," says lead author Dr Shijie Jiang, who now works at the Max Planck Institute for Biogeochemistry in Jena.

The scientists used explainable machine learning for the analysis. "First, we use the potential flood drivers air temperature, soil moisture, and snow depth as well as the weekly precipitation -- each day is considered as an individual driving factor -- to predict the run-off magnitude and thus the size of the flood," explains Zscheischler. The researchers then quantified which variables and combinations of variables contributed to the run-off of a particular flood and to which extent. This approach is referred to as explainable machine learning because it uncovers the predictive relationship between flood drivers and run-off during a flood in the trained model. "With this new methodology, we can quantify how many driving factors and combinations thereof are relevant for the occurrence and intensity of floods," adds Jiang.

Read more at Science Daily

Aug 27, 2023

New study examines historical drought and flooding on the Amazon River

Despite the rapid increase in severe flooding, a new paper by researchers from the U of A indicates recent floods and droughts in the Amazon River Basin may have not yet exceeded the range of natural hydroclimatic variability.

Extreme floods and severe droughts on the Amazon River have occurred more frequently in the last 40 years. Eight of the 12 most extreme floods in the 121-year streamflow record at Manaus, located on the Negro River, a tributary of the Amazon River, have occurred in just the last 14 years.

Natural climate variations, deforestation and anthropogenic climate change are all likely contributors to the recent Amazon River level extremes. Despite the rapid increase in severe flooding, a new paper by researchers from the U of A indicates recent floods and droughts in the Amazon River Basin may have not yet exceeded the range of natural hydroclimatic variability.

The American Meteorological Society published these recent findings by Daniela Granato-Souza, a post-doctoral student in geosciences, and David Stahle, a Distinguished Professor of geosciences, in a new paper titled, "Drought and flood extremes on the Amazon River and in northeast Brazil, 1790-1900."

Using tree-ring analysis to reconstruct rainfall totals in the eastern Amazon, along with historical documentary accounts of extreme flooding in Manaus and Santarem, Granato-Souza and Stahle found evidence indicating that Amazon River floods in 1859 and 1892 may have equaled or exceeded recent flooding.

The biggest difference between then and now, though, is the size of the population now living in the flood plain.

"There are millions of people residing in Manaus, the most populous city in northern Brazil, so there is a socioeconomic concern in these regions," noted Granato-Souza. "Usually, poorer people are seen living in risk areas, and with each flood they suffer the consequences of loss and illness. There is a 'normal' for the maximum level that the river reaches, but the most extreme floods exceed this threshold, and studies have shown that this is intensifying."

Granato-Souza added that while they found the recent extreme floods weren't unprecedented, examining the scale of past flooding provides a framework for imagining and anticipating the environmental and socioeconomic consequences of future floods.

And they would likely be devastating for a population living in high-risk areas.

Read more at Science Daily