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Exact(7)
Magnitudes were calculated by the method of Watanabe (1971).
Where unavailable in the literature magnitudes were calculated specifically for LaMEVE from the published volume data or VEI values.
Moment The values of the moment and the corresponding moment magnitudes were calculated according to the relation of Hanks and Kanamori (1979).
Normalized effect magnitudes were calculated as previously described.
Spectral magnitudes were calculated for 10 Hz-wide bins surrounding H2 and H4.
Local magnitudes were calculated using amplitudes measured on the horizontal components of simulated Wood Anderson displacement seismographs and the distance correction for the Main Ethiopian rift (Keir et al. 2006, 2011).
Similar(51)
Magnitudes are calculated from the maximum seismic wave amplitudes.
The magnitudes are calculated from data acquired at the closest three to ten stations.
Magnitudes are calculated from the maximum amplitude at the stations indicated by closed circles and closed triangles.
The difference between the magnitudes is calculated using (tau_{text{P}}^{ hbox{max} }), (tau_{text{c}}), and (tau_{{f{text{cwt}}}}) which are represented by solid gray circles, hollow black squares, and solid black triangles, respectively.
However, under more realistic setting of the smartphones, which is the scope of this study, for the arrangement where the sum of magnitudes is calculated from the sum of all axes acceleration vibration, there are mixed results of the R2 values in the total range of frequency (0 to 50 Hz).
Related(20)
magnitudes were estimated
magnitudes were computed
degrees were calculated
significance were calculated
scale were calculated
importance were calculated
magnitudes were chosen
magnitudes were dropped
magnitudes were identified
magnitudes were increased
magnitudes were assessed
magnitudes were obtained
magnitudes were performed
magnitudes were used
magnitudes were selected
magnitudes were seen
magnitudes were lost/gained
magnitudes were based
magnitudes were observed
magnitudes were related
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