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Bivariate distribution of (a) river floods and wildfires, (b) river floods and wildfires, and (c) heatwaves and wildfires, across 50-year time periods representing the early industrial period (1861–1910), the present day (1956–2005), and the end of the century (2050–2099) under RCP2.6, 6.0, and 8.5. The marginal distributions of each extreme event (per scenario), based on the KDE method , are shown along the top and right axes of the plots. The contours (dotted lines) illustrate smooth estimates of the underlying distribution of co-occurring extremes. The 68th percentile contour, which envelops data within 1 standard deviation to either side of the mean, is used per scenario to show a generalized view of the distribution of the percentage of area affected by co-occurring extremes per year during the respective scenarios.

Bivariate distribution of (a) river floods and wildfires, (b) river floods and wildfires, and (c) heatwaves and wildfires, across 50-year time periods representing the early industrial period (1861–1910), the present day (1956–2005), and the end of the century (2050–2099) under RCP2.6, 6.0, and 8.5. The marginal distributions of each extreme event (per scenario), based on the KDE method , are shown along the top and right axes of the plots. The contours (dotted lines) illustrate smooth estimates of the underlying distribution of co-occurring extremes. The 68th percentile contour, which envelops data within 1 standard deviation to either side of the mean, is used per scenario to show a generalized view of the distribution of the percentage of area affected by co-occurring extremes per year during the respective scenarios.

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Co-occurring extreme climate events exacerbate adverse impacts on humans, the economy, and the environment relative to extremes occurring in isolation. While changes in the frequency of individual extreme events have been researched extensively, changes in their interactions, dependence, and joint occurrence have received far less attention, partic...

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... One hazard changes environmental parameters, resulting in an increased probability of another hazard occurring 38 . For instance, heatwaves increase the probability of wildfires in East Africa 40 . ...
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... CC BY 4.0 License. climate events (Muheki et al., 2024), and project future indices regarding water scarcity in the context of CC and societal changes (Yin et al., 2020). ...
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... Extreme climatic events, like droughts, are increasing in frequency and severity with anthropogenic climate change (Pörtner et al. 2023). Droughts pose a significant threat to rural communities and, in particular, pastoral communities throughout the Greater Horn of Africa (Megersa et al. 2014;Muheki et al. 2024). Droughts have long-term consequences not only for the environment and human health, but also for livelihoods, which trigger a cycle of health deterioration (WHO 2023). ...
... The Greater Horn of Africa, an area characterized by extreme heat and low rainfall, is particularly impacted by climate change, including both drought and flooding, with projections indicating that climate change will exacerbate existing vulnerabilities (Anyah and Qiu 2012;Muheki et al. 2024;Tierney, Ummenhofer, and Demenocal 2015). Between October 2020 and April 2023, the Greater Horn of Africa, including northern Kenya, experienced the most severe drought in 40 years. ...
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