2014
DOI: 10.1007/s11200-014-0825-2
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Application of P-wave Mwp magnitude to earthquakes for tsunami early warning in and around South-Western Turkey

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Cited by 5 publications
(2 citation statements)
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“…The main issue is the selection of the time window on seismograms to calculate the P-wave moment magnitude. Either using a fixed time window or a moving window cause some problems because it is very difficult to catch the right source duration at moment magnitude calculations [15,16]. To overcome this type of problem, this study proposed the use of a time window that starts 10sec before P-wave arrival and finishes at S-wave onset for each seismogram.…”
Section: Methodsmentioning
confidence: 99%
“…The main issue is the selection of the time window on seismograms to calculate the P-wave moment magnitude. Either using a fixed time window or a moving window cause some problems because it is very difficult to catch the right source duration at moment magnitude calculations [15,16]. To overcome this type of problem, this study proposed the use of a time window that starts 10sec before P-wave arrival and finishes at S-wave onset for each seismogram.…”
Section: Methodsmentioning
confidence: 99%
“…These calculations are based on farfield recordings of tsunamigenic earthquakes. In contrast, Hishorn et al [8], Tezel and Yanik [9], and Tezel [10] showed that the Mwp could be calculated using local and regional earthquakes. Although these studies used weak-motion velocity seismograms from broadband seismometers, Tezel [11] used strong motion records for the calculations.…”
Section: Introductionmentioning
confidence: 95%