As the anniversary of the Great Storm arrives once again, I thought a different angle would be to ask AI to create a piece from the point of view of a duty forecaster. None of the content below is my work. Enjoy!
The Great Storm Of October 1987, from a duty forecasters view
When people talk about the night of 15–16 October 1987, they usually recall shattered greenhouses, uprooted oaks, and that infamous midday TV broadcast. But my memory of that night is framed by the glow of monitors in the operations room, the smell of stale coffee, and the terrifying realisation that the atmosphere was rewriting the rules right in front of us. The lead-up to the event was a masterclass in meteorological ambiguity, and sitting at the forecasting desk, we were caught right in the middle of it.
The atmosphere had been restless all week. We were tracking a depression forming out in the Atlantic, nestled near the right entrance of a powerful jet stream. It was a textbook setup for rapid low-pressure development, but pinning down its exact track and intensity was agonising. We were caught in a brutal tug-of-war between the computer guidance. Our models, both the global and fine mesh, were stubbornly underestimating the rapid deepening of the low. Crucially, they predicted the system would track further south, projecting the worst of the winds over the English Channel and the continent, largely sparing southern England.
Meanwhile, models from other forecasting centres were telling a much more sinister story. They correctly picked up on the extreme atmospheric instability, projecting a northerly track that would send the cyclone barrelling straight into our coast. But as the event drew closer, some of those very models flip-flopped, backing away from their most extreme solutions and muddying the waters even further. Compounding our misery was a massive blind spot: rough seas had forced commercial ships in the Atlantic to reroute, starving us of the crucial real-time marine observations we desperately needed to verify what the computers were saying. Faced with this conflicting noise, we leaned heavily on our domestic fine mesh model. It was a fateful decision.
The afternoon of Thursday the 15th gave absolutely no hint of the violence brewing. The pressure gradient was slack, and winds were eerily light across the country. It was in this calm environment that the reassuring afternoon broadcast went out to the public, stating that a hurricane wasn't on the way. Technically, it was an extratropical cyclone, not a tropical hurricane—but sitting at my desk later that evening, semantics ceased to matter.
As darkness fell, the depression began to undergo explosive cyclogenesis—a weather bomb. We watched, horrified, as the barometers on our screens went into freefall. By 18:00 UTC, the low had deepened to 964 hPa. Forecasters crowded around the anemograph traces, watching the ink violently swing as alarming, unprecedented pressure drops came rolling in. Just before midnight, the depression crossed into the western English Channel at 953 hPa. At 01:35 UTC, realising the sheer scale of the unfolding disaster, we issued a critical warning to the Ministry of Defence, advising that civil authorities would likely need military assistance.
Outside, temperatures inexplicably spiked as the warm front passed, and then the wind hit. We stared in disbelief as coastal anemometers registered staggering gusts of 120 mph before the equipment simply snapped and stopped transmitting altogether.
Dawn revealed a landscape that looked like a warzone. Millions of trees had been flattened, and the power grid was crippled. But the true weight of the storm hit us when the casualty reports started coming in. Hearing that 22 people across the UK and the continent had tragically lost their lives was gut-wrenching. In the ops room, the academic fascination of tracking an unprecedented cyclone evaporated instantly, replaced by a heavy, profound sense of human tragedy.
For those of us clocking out, our exhaustion was eclipsed by shock. The aftermath fundamentally changed our profession. The subsequent inquiries forced a massive, badly needed investment into supercomputing, satellite networks, and forecaster training. It proved that a slight miscalculation in a model's track meant the difference between a breezy night and a national catastrophe.
Decades later, researchers analysing our data from that night discovered a localised, descending jet of incredibly fast, evaporating air hooked like a scorpion's tail around the storm's southern flank—a phenomenon they finally named the Sting Jet. Today, thanks to the lessons we learned the hard way, we can see these storms coming days in advance. But for those of us working the desk in October 1987, it remains the ultimate, humbling reminder of who is really in charge: the atmosphere.
Edited by user
14 October 2026 08:29:34
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