In this Story
- When the Heat Turns Into a Grid Problem
- The Real Problem: Heat Stresses Every Part of the System at Once
- The Hitzeflaute: The Summer Cousin of the Dunkelflaute
- Hidden Capacity: Where High-Resolution Weather Data Changes Outcomes
- Speed and Situational Awareness: From Slow Burn to Sudden Chaos
- AI Enters the Control Room: The Meteomatics MCP Connector
- What This Means for Grid Operators
- Q&As
- Transcript
Presented by: Meteomatics and Heimdall Power
Date: July 15, 2026
Duration: 52 minutes
Participants:
- Meteomatics expert: Dr. Matthias Piot (Senior Energy Meteorologist)
- Meteomatics expert: Keanu Giebels (Account Executive, Energy & Utilities)
- Heimdall Power: Brian Berry (Chief Product Officer)
- Moderation: Candice Thompson (Customer Success Manager, Meteomatics)
When the Heat Turns Into a Grid Problem
The grid was built for a climate that no longer exists.
For years, the winter Dunkelflaute — cold, dark, windless days — dominated the conversation about renewable-driven risk. But the summer of 2025 exposed the other side of the problem. Record-breaking European heat, collapsing wind, aging infrastructure and surging cooling demand combined to push the grid to its limits, at the exact moment supply was least able to respond. In the latest webinar, "The Temperatures Are Rising: Building Network Resilience in a Warming Climate," experts from Meteomatics and Heimdall Power weighed in.
"You can go back to at least 1940, even beyond, and you won't find such a warm June in our history," said Dr. Matthias Piot from Meteomatics.
The trend is structural. And it is exposing how fragile the grid becomes when heat, demand and generation all move in the wrong direction at once.
The Real Problem: Heat Stresses Every Part of the System at Once
Extreme heat does not create a single, isolated failure. It attacks the grid from multiple directions simultaneously.
During the June heat wave, France experienced temperatures up to 17°C above normal, with national weather services issuing red alerts across large parts of Central Europe. The consequences were immediate:
- Italy suffered eight power failures within 24 hours, driven by air-conditioning load on aging infrastructure
- A transformer in Western France exploded from overheating, leaving 100,000 households without power for days
- Wildfires in Southern France added further outages
At the same time, demand climbed while supply shrank. French demand rose 10–12 GW purely from air conditioning — the equivalent of roughly ten nuclear reactors — while French nuclear output was constrained because river temperatures exceeded 28°C, making it impossible to discharge cooling water. UK gas plants faced similar restrictions. Across Europe, the heat added an estimated 20–35 GW of cooling load.
"That means more stress on the grid, less energy being transmitted through the lines — the ampacity — and more stress on aging infrastructure," Dr. Piot explained.
The Hitzeflaute: The Summer Cousin of the Dunkelflaute
If the winter risk is the Dunkelflaute, the summer equivalent is what the Meteomatics team calls the Hitzeflaute — sustained excessive heat, little to no wind, and high solar generation during the day.
"It's hot, and the air isn't moving. That's actually it," said Keanu Giebels from Meteomatics.
The dynamic is deceptively simple but financially brutal. Solar keeps prices low, even negative, at midday. But the moment the sun sets, solar disappears, demand stays high, and there is no wind to lean on. Operators are left scrambling for capacity in an "evening cliff," with intraday prices swinging €300–500 in a single day.
The June event in Germany illustrated the scale:
- German demand climbed from ~53 GW to ~58 GW; French demand rose almost 20%, from ~44 GW to ~52 GW
- Germany peaked above €700/MWh, France around €430, Spain around €185
- EDF was forced to pull 8% of France's nuclear generation due to warm rivers
- German onshore wind collapsed from over 22 GW to just 1.3 GW — a 90%+ drop — precisely when the grid needed it most
The same heat-and-calm combination also erodes the thermal headroom on lines and transformers. As Giebels put it, the real question is "how you find flexibility when the weather's working against you on every front at the same time."
Speed and Situational Awareness: From Slow Burn to Sudden Chaos
Not every event unfolds slowly like the Hitzeflaute. On June 19, the Netherlands went from calm to chaotic in hours: temperatures above 30°C in the evening, followed by severe thunderstorms and over 180,000 lightning strikes.
This is where Meteomatics' visualization tool, MetX, proved its value. In a single view, operators could track heat warnings, thunderstorm movement, lightning strikes and a live grid map of Dutch overhead lines that changed color as wind-gust thresholds were crossed.
"It's about being able to act proactively on weather events instead of reactively," said Giebels. "In today's landscape, speed is really turning into the key."
AI Enters the Control Room: The Meteomatics MCP Connector
The newest addition to the Meteomatics suite is an MCP (Model Context Protocol) connector, which links the weather API directly to AI agents such as Claude, ChatGPT or Copilot.
"Think of AI as your computer, and the MCP connector as a USB stick full of information," Dr. Piot explained. "You can plug a huge amount of Meteomatics data in — and it can be set up within ten minutes."
In the demos, the team used natural-language prompts to build interactive HTML dashboards on the fly — for example, mapping the impact of the French heat wave using the high-resolution EURO1k model, combined with a CSV of the French grid network. Crucially, the prompt instructs the model to pull only from the Meteomatics API rather than fabricating or scraping open-source data, keeping the output trustworthy.
"I was skeptical at first about what I'd actually do with an MCP server," Giebels admitted. "But the answer is obvious — there are endless possibilities. A grid or renewable-asset operator can add any set of locations, assets and parameters and understand the risks they face at different times of year."
What This Means for Grid Operators
The takeaway is not that weather is becoming more important. That has already happened. The real shift is this:
- Heat now stresses generation, transmission and demand simultaneously
- The Hitzeflaute is becoming a defining feature of summer, not an anomaly
- Static ratings leave real, usable capacity unclaimed on the lines
- Speed and situational awareness increasingly separate proactive operators from reactive ones
Or more simply: the heat waves don't wait — and neither can the grid. The advantage is no longer just having weather data. It is having the right weather signal, at the right resolution, at the moment it matters.
Q&As
Question:
Normally dynamic line rating (DLR) is used to gain capacity when a line is cooler than the static model assumes. During a heat wave, isn't it the opposite — you learn you have less capacity, because the real temperature is higher than the value used in the static calculation?
Answer:
It's a fair question, and the short answer is that DLR still provides value — because of wind.
Of the three factors that affect a line — solar radiation, ambient temperature, and wind — wind has by far the greatest impact, but it is also the hardest to capture accurately. So even in extreme heat, if there is wind, you may get relief that a static rating would never reveal.
You are right that during a heat wave the temperature side will often be strained and can bring your rating down. If there is no wind and ambient temperature is high, you will see a loss of capacity, and that isn't congestion relief. But it is far better to understand that risk than to be blind to it. Knowing your true limit lets operators take the right action — including clamping a line down when necessary — rather than assuming a headroom that isn't there. It's better to know it than not to know it.
Question:
With hotter, drier summers and strong El Niño events, wildfire risk is rising. Are you seeing more customers ask about this, and does Meteomatics offer parameters to track wildfire and its spread?
Answer:
Wildfire is a huge topic, especially in the US, where utilities have gone bankrupt over liability claims for fires started by their assets. There is no silver bullet — it's a multifaceted problem spanning prevention (understanding when weather turns dry and hot), infrastructure decisions (overhead lines versus underground cables, vegetation management), and operations (keeping the grid running even when power must be switched off to reduce risk).
On the data side, Meteomatics offers wildfire-relevant indices such as the Fosberg Index, alongside parameters like wind, relative humidity, temperature and soil dryness, all of which can be combined into a MetX dashboard or accessed via the MCP connector, with custom thresholds and alerting.
Two important caveats. First, dryness alone doesn't cause fire — you need an igniter (human or natural, such as lightning) and you have suppressors (precipitation, low wind) that limit spread. Combining ignition sources, suppressors and weather conditions lets you identify where risk is highest. Second, the tool identifies wildfire risk, not the tracking of an active fire's spread — that is outside our domain.
The real power comes from combining data sources: wildfire-fuel APIs and satellite APIs bring one picture, and layering the Meteomatics MCP on top adds the weather dimension. Together they give the full picture that no single source can.
One physical detail worth noting: even a small, controlled fire passing under a line is disruptive, because the smoke is full of conductive carbon and can cause a flashover. Operators often respond by disabling auto-reclose and preemptively managing the line. This is also linked to the sag effect — during the June 2024 Balkans heat, cables expanded and sagged low enough to risk flashover with vegetation, contributing to a major regional blackout.