How Does an Earthquake Early Warning Work?
An earthquake early warning is not a prediction. Sensors near the epicentre detect the fast, weak P-wave, software estimates the shaking from those first seconds of data, and an alert reaches phones ahead of the slower, damaging S-wave. The gap between the two waves is the warning: seconds near the epicentre, up to a minute further out.
That distinction decides whether the public trusts the system. Residents who believe an earthquake was forecast will treat a short warning as a failure, and a false alarm as proof the system does not work. Explaining the physics converts the alert from a broken promise into a head start. The material to leave in the source document is a specific warning time for a specific location — it depends on the epicentre, and publishing a number invites the complaint that it did not arrive.
The sequence runs across seven scenes: two on the two wave types and why one outruns the other, one on how the estimate is made from partial data, one on why the warning is shorter near the epicentre, two on what the seconds are actually enough for, and one on what the alert sounds and looks like on a phone.

