The Mercury News Weekend

ShakeAlert

- To download the app, go to myshake.berkeley.edu.

“We learn something new from every opportunit­y to do something like this,” de Groot said. “Of course, today was a learning experience. Yesterday was a learning experience for us as well.”

State officials say the goal of the ShakeOut was to encourage people to practice earthquake safety and to remind residents to keep their emergency earthquake kits well stocked. About 10 million people were expected to participat­e throughout the state, including schoolchil­dren and many office workers.

A simple time zone mixup was to blame for the erroneous early-morning test alerts, de Groot said.

The messages were delivered at 10:19 Coordinate­d Universal time, rather than Pacific time.

“It was just a simple twist in the code,” de Groot said. He added that the problem since has been corrected.

A previously scheduled alert for the correct time of 10:19 a.m. PDT was still sent as planned. However, some people who received the early-morning message did not get the second message later in the day.

Both the errant predawn messages, as well as the 10:19 a.m. follow-up messages, were only sent to people who had downloaded the MyShake app and who had successful­ly installed the program on their phones. More than 1 million people across the West Coast have installed the app, though it's unclear how many people have completed the setup process, de Groot said.

In the event of a real earthquake, additional messages also could be sent via other means, including through Google and through cell towers, similar to how Amber Alerts are issued. However, those extra messages depend on the severity of the quake. For example, warnings will only be sent over all platforms during a quake with a magnitude of 5.0 or greater.

The alerts came a day after the 34th anniversar­y of the 1989 Loma Prieta quake and marked the second straight day of unexpected warnings for people across the Bay Area and the Sacramento River delta after a 4.2 magnitude temblor struck Wednesday morning near the town of Isleton. The initial alert for that rattler suggested the quake was a magnitude 5.7 — 31 times stronger than the actual quake that struck.

The reasons for that incorrect reading were twofold, de Groot said. And both relate to the location of undergroun­d sensors meant to detect the first stirrings of a quake.

Typically, notificati­ons are based on the sensors' measuremen­t of the first wave to be released from an earthquake, otherwise known as a compressio­nal, or “p,” wave. On Wednesday, however, a sensor was remarkably close to the earthquake's epicenter — meaning it also appeared to pick up hints of the quake's more powerful shear, or “s,” wave, skewing the sensors' initial readings.

De Groot likened the phenomenon to the difference between observing lighting at different distances. From far away, a pause exists between a lighting bolt's flash and the ensuing thunder. Yet when a bolt strikes nearby, thunder can rattle the air almost simultaneo­usly.

“That's kind of what happened in this event, is that the thunder and the lightning arrived at the same time,” de Groot said.

In addition, the quake took place in the Sacramento Delta — an area known for soft, waterlogge­d soils that can amplify shaking, even during a mild or moderate quake.

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