2 weeks ago

Why Europe’s Extreme Summer Heat Is Not Just El Niño

Why Europe’s Extreme Summer Heat Is Not Just El Niño
Explained: El Nino's Role in Europe's Extreme Summer Heat and Wildfires · NDTV

Belgium recently experienced its largest recorded wildfire.

The fire burned forests and peatland after a very hot period.

Hundreds of people had to leave nearby areas for safety.

Rain and cooler weather later helped firefighters.

Other parts of Europe also faced heat, drought, and wildfires.

El Niño can affect weather around the world, but its effect on European summers is usually weak and indirect.

Experts say dry soil, Atlantic conditions, stuck high-pressure systems, and long-term climate change are more important for Europe’s summer heat.

El Niño can still make a hot year worse when it occurs alongside an already warmer global climate.

Key facts

Belgian wildfire area
Approximately 3,000 hectares of peatland and pine forest burned.
Peak temperature
Temperatures reached 37°C (98.6°F) during the heatwave.
Evacuations
About 600 residents and tourists were evacuated from Waimes and Butgenbach.
Emergency response
More than 250 emergency personnel, supported by military units and others, fought the fire.
European river levels
Dry conditions reduced water levels in the Seine, Rhine, and Danube.
Wildfire emissions
Emissions in France and Spain were reported to be well above average for that time of year.
Main El Niño assessment
Its influence on European summer weather is indirect and weaker than regional atmospheric and oceanic drivers.

Quotes

John Kennedy

Head of climate information at the World Meteorological Organization

“What we have seen over the last few months is the combined effect of long‑term warming with a persistent pattern of alternating high‑ and low‑pressure systems stretching across the Northern Hemisphere.”
NDTV

Prof. Martina Zelenakova

Professor at the Technical University of Kosice, Slovakia

“El Nino does not work as a simple rule "El Nino = warm and dry Slovakia." Its influence is transmitted through changes in atmospheric circulation over the Atlantic and Europe and is relatively weak compared to the influence of the NAO, blocking high‑pressure areas or climate change itself.”
NDTV

Sources

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