In April 2024, Taiwan faced a powerful earthquake, measuring 7. 4 on the magnitude scale. The Central Weather Administration's early warning system had a rough time with it. The system initially guessed the earthquake's strength at 6. 8, all within 15 seconds. This quick guess was way off, and it led to no alerts for the Taipei area. People there felt the quake strongly, with shaking that reached level 5 on the intensity scale. This mistake sparked a lot of complaints. People wanted to know why the warning system failed them.

The issue of figuring out an earthquake's size quickly is a big challenge. Scientists are always looking for better ways to do this. In this case, researchers tested a new method using low-cost sensors. They looked at something called cumulative absolute absement. This is a fancy way of saying they measured how much the ground moved in total. They compared this with the methods the current system uses. The current system looks at the biggest vertical movement and the average time between waves.

The new method seemed to give a closer guess to the final magnitude. But it also had more uncertainty. The current methods were more stable. One interesting thing they found was that the direction of the earthquake's rupture mattered. When they only used sensors from the north, they overestimated the size. When they used only southern sensors, they underestimated it. This shows that where the sensors are placed is super important.

The new method seemed to handle the direction of the rupture better. This could make it a good choice for future warning systems. The big takeaway is that picking the right measurements and placing sensors correctly can make a big difference. This can help make early warning systems faster and more accurate. Faster and more accurate warnings can save lives and reduce damage.

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