Skip to content

E9: Dry spells and downpours

Climate Science, Atmospheric Science and Meteorology podcast with Mathew Barlow

Ask MIT Climate, Hosted by Madison Goldberg

About

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

More from this series

More from Ask MIT Climate

All episodes

We use cookies for analytics.