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• W2013203422 abstract "[1] Pd is the peak amplitude of displacement in the first three seconds after the arrival of the P wave. We investigated the attenuation of Pd with the hypocentral distance R in southern California as a function of magnitude M, and obtained the following relationship: log (Pd) = −3.463 + 0.729 × M − 1.374 × log (R) ± 0.305. Given an earthquake location determined by the P-wave arrival times at stations close to the epicenter, this relationship can be used to define a so-called “Pd magnitude” of earthquakes. Our result shows that for earthquakes in southern California the Pd magnitudes agree with the catalog magnitudes with a standard deviation of 0.18 for events less than magnitude 6.5. Therefore, Pd is a robust measurement for estimating the magnitudes of earthquakes and has practical application in earthquake early warning systems." @default.
• W2013203422 created "2016-06-24" @default.
• W2013203422 creator A5048406699 @default.
• W2013203422 creator A5090517968 @default.
• W2013203422 date "2006-01-01" @default.
• W2013203422 modified "2023-10-16" @default.
• W2013203422 title "Magnitude estimation using the first three seconds P-wave amplitude in earthquake early warning" @default.
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• W2013203422 doi "https://doi.org/10.1029/2006gl026871" @default.
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