Fig. 16From: Seismic signature detection during the 2018 Anak Krakatau flank collapse and tsunami using seismic amplitudes from regional-scale monitoringIllustrated procedure for real-time event detection. a Initial detection using averaged \(B\). b Identification scheme to distinguish seismic events using \(C\) and \(\gamma\) values, along with the thresholds \({\Gamma }_{1}\), \({\Gamma }_{2}\), and \({\Gamma }_{3}.\) Green rectangle denotes the preferable result where \({\Gamma }_{1}<C<{\Gamma }_{2}\) and \(\gamma >{\Gamma }_{3}\). Colors are illustrative and do not represent actual \(C\) valuesBack to article page