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A trigger-data classification based only on arrival time differences appears to pose a fundamental obstacle for separating trigger data from multiple earthquakes within such short distances.
The system determines hypocenter locations and magnitudes using trigger data from these strong-motion seismometers.
This successful isolation resulted from the use of observed velocity amplitudes in classifying trigger data.
The trigger data handshake mode uses the same scheme as in the simple handshake mode, but additionally the current trigger data are transferred on the trigger line: after the trigger has been de-asserted, the trigger number is clocked out.
Cases with prediction scores of <10% occurred due to the misclassification of trigger data derived from multiple simultaneous earthquakes.
The trigger data are updated every 4 s and hold the peak value until being reset at a fixed time.
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The instrument was set to trigger data-dependent MS/MS acquisition of the three most intense ions detected during the MS survey scan when total ion current per MS survey scan exceeded 5.0×105 counts.
The proposed solution leads to a new event-triggering data transmission mechanism, which drastically differs from the existing event-triggered control results.
(a) Time-triggered data.
These data are triggered data which are recorded once the acceleration exceeds the level predetermined for each station.
However, only a small portion of the triggering data can be relayed because the available telemetry data are limited.
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