A European drought crisis is intensifying due to climate change, with extreme heat driving rapid soil and water evaporation across the continent.

Quantitative findings show soils are extremely dry five times more likely in western Europe and 11 times more likely in eastern Europe today versus a 1.4°C cooler scenario, with evaporative demand about 80 times higher in western Europe from April to June.

Droughts begin to emerge at around 1.4°C of warming, and if global temperatures reach 2.8°C, intense evaporation-driven droughts could become regular, underscoring the need for rapid emission reductions.

The initial translation of findings was AI-generated but later verified by a human editorial team.

Historical crop losses could push up food prices and disproportionately affect low-income households.

The World Weather Attribution study is a consortium that includes Imperial College London, KNMI, ETH Zurich, LSE, and other institutions, with participation from the German Weather Service for the current study.

A wet winter followed by a dry spring created conditions that heightened forest-fire risk.

UN Climate Chief emphasizes that worsening droughts affect food prices, energy systems, and inland transport, highlighting broader societal impacts of the climate crisis.

Researchers note that higher temperatures worsen drought risk even with unchanged or increased precipitation, due to accelerated atmospheric moisture drawdown from soils.

The analysis compares current conditions with a world 1.4°C cooler since 1850–1900, focusing on rainfall deficits, potential evapotranspiration, and soil moisture across twelve European countries.

Ongoing emission trajectories will determine how frequently and intensely droughts recur, potentially making them regular events.

Under current trends, conditions similar to April–June are unlikely to improve in the near term, with droughts estimated to recur roughly every five years and potentially double in likelihood at 2.8°C of warming.