{"id":1189,"date":"2022-07-28T09:13:10","date_gmt":"2022-07-28T08:13:10","guid":{"rendered":"https:\/\/research.reading.ac.uk\/lemontree\/?p=1189"},"modified":"2022-08-09T10:31:56","modified_gmt":"2022-08-09T09:31:56","slug":"extreme-heat-in-the-uk-and-wildfires-why-we-should-expect-it-to-happen-again","status":"publish","type":"post","link":"https:\/\/research.reading.ac.uk\/lemontree\/extreme-heat-in-the-uk-and-wildfires-why-we-should-expect-it-to-happen-again\/","title":{"rendered":"Extreme heat in the UK and wildfires: why we should expect it to happen again"},"content":{"rendered":"
<\/p>\n
On Friday 15th July 2022, the UK Met Office issued its first ever Red Warning for exceptional heat. Over the following two days, temperatures across the UK broke records, reaching 40.3\u00b0C in England, 37.1 \u00b0C in Wales and 34.8\u00b0C in Scotland. The weather drove a sharp response in wildfire risk, with major wildfire incidents declared in London and Surrey.<\/p>\n
Media have reported that the fires were driven by the extreme heat, but the specifics of this relationship are important to understanding the changing landscape of wildfire risk in the UK and globally.<\/p>\n
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Higher daily maximum temperatures result in a sharp increase in wildfire risk – with all other factors being equal. Consequently, this results in more wildfire starts, more rapid wildfire spread, and hotter fires. All of which challenge fire services.<\/li>\n
The frequency with which daily temperature extremes occur will increase exponentially with shifts to the global mean temperature – resulting in serious changes to wildfire risk globally.<\/li>\n<\/ol>\n
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Climate distribution<\/u><\/h2>\n
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Extreme heat will become more common as the probability of temperature maximums fall exponentially at high values. This means small shifts to the average temperature can have a huge impact on how often we might see extreme highs – such as 40\u00b0C in the UK.<\/p>\n
Fig 1: As the mean is shifted, high temperature values increase exponentially in frequency. (\u00a9Theo Keeping)<\/p>\n
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Wildfire response to heat<\/u><\/h2>\n
For a wildfire to spread, there must be dry and sufficient fuel. Higher temperatures cause more rapid and complete drying of vegetation. Dry vegetation ignites more easily and fire spreads more rapidly through it, meaning a small blaze can quickly get out of hand. In addition, the heat of wildfires is also increased with drier fuel, making it harder for fire services to manage the blaze.<\/p>\nFig 2: Example of the expected temperature for different probabilities of a fire starting using fire occurrence and weather data from the United States. (FPAFOD, PRISM) (\u00a9Theo Keeping)<\/figcaption><\/figure>\n
Management<\/u><\/h2>\n
Many regions for which wildfire has not been a serious historic risk will be forced to confront a regime in which fires are much more frequent and severe. We will need to employ strategies such as managing fuel loads by clearing vegetation understories, allowing natural regrowth and ensuring easy access routes. This will not only help reduce the speed and intensity of future wildfires. Furthermore, it will provide quicker access for fire services, which is essential for stopping fire spread.<\/p>\n
By LEMONTREE PhD candidates Theo Keeping and Olivia Haas.<\/p>\n","protected":false},"excerpt":{"rendered":"
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