As Europe battles severe flooding, we ask what role is climate change playing in extreme rainfall? Will floods get worse as global temperatures rise? These five visualizations will help you understand the connections.
Severe flooding has forced tens of thousands to evacuate their homes as wide regions of Austria, the Czech Republic, Poland and Romania have been hit by days of heavy rainfall.
It is the latest of several extreme floods this year. In Europe, thousands were forced to evacuate this summer in southern Germany. Elsewhere in the world, the United Arab Emirates and Oman experienced the heaviest rainfall since records began. Deluges in Kenya claimed numerous lives and triggered landslides. And in Brazil, floods damaged an area equivalent in size to the UK and displaced over half a million people.
Whereas coastal flooding is largely driven by winds and high tides, river, groundwater and flash flooding are all linked to heavy rainfall. Rising global temperatures, caused by burning fossil fuels, is making rainfall more frequent and severe across most parts of the world.
What is the science behind extreme flooding?
Hot air holds more moisture.
Modeling precipitation patterns is a complex process, but it has one clear underlying physics principle: hot air holds more moisture.
Greenhouse gases released into the atmosphere act like a blanket on the earth, trapping heat and causing temperatures to rise. This leads to a more rapid evaporation of water on land and at sea, meaning that when it rains, there is more water to release. And when a huge amount of rain is dumped onto earth in a short space of time, this can lead to flooding.
Air’s capacity to hold moisture rises by 7% with every rise of 1 degree Celsius. Since the pre-industrial era, global air temperatures have increased by around 1.3 degrees Celsius.
Temperature rises also make more precipitation fall as rain instead of snow which can make high altitude regions vulnerable to flooding and landslides. A 2022 study published in the science journal Nature found that in snowy, high-elevation parts of the Northern Hemisphere, rainfall extremes increased by an average of 15% per 1 degree Celsius of warming.