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Climate scientist Mathew Barlow explains why warming can intensify both drought and extreme rainfall. The episode follows water through a warmer atmosphere, connecting increased moisture capacity and evaporation with dry soils and stronger downpours. It distinguishes changes in average conditions from the most damaging extremes and discusses why infrastructure faces growing flood risks.

Topics

droughtextreme rainfallwarmer atmospheremoisture capacityevaporationdry soilsdownpoursflood risks

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