If lightning strikes a hundred miles from the North Pole, and no one is around to hear it, does it make a sound? Yes, because there’s a global array of sensors that’s always listening, pinpointing lightning strikes in time and space from as far away as 6,000 miles.

In June and this past weekend, the North Pole played host to rare thunderstorms, an event that may become less rare as climate change ramps up. And it would have gone entirely unnoticed by faraway humans if it weren’t for the assistance of a company called Vaisala, which operates the sensor network and uses it to triangulate a lightning strike, feeding the data to outfits like the National Weather Service. “This is a relatively new system, and so our ability to detect lightning that far north has drastically improved over the last 5 to 10 years,” says Alex Young, a meteorologist with the National Weather Service in Fairbanks, Alaska. “As opposed to: who knows if an event like this happened 30 years ago?”

Matt Simon covers cannabis, robots, and climate science for WIRED.

First we need to talk about how lightning forms. When the Sun heats the Earth's surface, air and moisture rise and create water droplets. With enough solar energy, the warm, wet air keeps rising and rising, while the same time, cold air in the system is sinking—leading to a swirling mass called a deep convective cloud, which builds electrical charges that escalate into lightning. Usually Arctic air doesn’t hold enough heat to get all that convection. But in these times of climate change, nothing is normal anymore.

Luckily for Vaisala, lightning betrays itself in a number of ways. We humans know it by the flash of light and the deafening sound, but what our bodies don’t notice is that the massive electrical current of a lightning strike generates radio bursts. For a fleeting moment, a lightning bolt works like a giant, rambunctious radio tower. “If you have a lightning discharge that hits the ground, you might have a channel of charge that's a few miles long,” says Ryan Said, a research scientist at Vaisala. “And that essentially acts as a temporary antenna in the sky.”

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Still, if it weren’t for a quirk in our atmosphere, this signal would be difficult to detect. But the ionosphere—an ionized layer in Earth's upper atmosphere—reflects a significant amount of the radio signal back to the ground for Vaisala’s devices to detect. Think of these like bigger, more sensitive versions of a loop antenna for receiving AM broadcasts. “If we have a sensitive enough receiver, we can detect these radio emissions at global distances,” says Said. “That's how, with dozens of receivers around the world, we can monitor lightning anywhere, including up into the Arctic.” (See above for a visualization of strikes around the world.)