Here we present updated analyses showing.

Verkkofor our analysis, we used the era5 climate variable hourly air temperature at 2 m above the surface gridded at a 31 km (0. 28125Β° at the equator).

Verkkothe extremes considered include temperature extremes, heavy precipitation and pluvial floods, river floods, droughts, storms (including tropical cyclones), as well as.

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Verkkoour findings reveal that dtrs are projected to increase because some nighttime hot extremes with their temperature lower than 21 Β°c are excluded.

Verkkothis study shows that temperature variability is key to explaining the highly heterogeneous trajectories of future extremes and their rapid intensification.

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