13-06-2025 Lightning Event

News / 13-06-2025 Lightning Event

Lightning has been detected!

On Friday the 13th of June 2025, the low pressure system located to the West of Ireland set up strong southerly flow of warm and humid air which destabilised over Northwest Europe, releasing substantial amounts of Convective Available Potential Energy (CAPE). The resulting convective system produced frequent lightning and travelled over Nantes and into Normandie, before following the coastline of Northern France. It then travelled north over the Channel, hitting areas of Kent and East Anglia.

The Met Office surface pressure chart for 13/06/2025 at 18:00 UTC.

Using lightning data from METEORAGE, in the 24-hour period of 06:00 13/06/2025 to 06:00 14/06/2025, there were 358,362 strikes recorded in WeatherQuest’s custom domain, which covers areas of Northern France and the British Isles. This was the most amount of recorded lightning in the domain since our records began, over 63,000 more than the second most active 24-hours.

A graph showng the number of lightning strikes each day from 01/01/2017 to 13/06/2025, with 13/06/2025 highlighted as having the highest.
The number of lightning strikes in WeatherQuest’s custom domain each day (06:00 – 06:00 24-hour period) from 01/01/2017 to 13/06/2025.
A heat map showing where the most lightning strikes occurred.
A heat map showing where lightning strikes were concentrated on the night of 13/06/2025 – 14/06/2025.

There are two different types of lightning, Intra-Cloud (IC) and Cloud-to-Ground (CG). Intra-cloud means that the lightning did not reach earth but instead struck through the cloud itself. Determining the type of lightning strike is achieved by analysing its electromagnetic signal discharge, with IC and CG both having different signals. The lightning during this 24-hour period was mainly IC (93% of total), but despite this, 25,621 strikes were CG, a quarter of which happened over the French city of Rouen, and its surrounding area (see the heat map above)!

A map showing the dispersion of lightning strike type over East Anglia and the Southeast.
The dispersion of lightning strike type over East Anglia and the Southeast.

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