An important component of the CTBT monitoring system is the 11-station hydroacoustic network designed to monitor the oceans for unannounced underwater explosions. Explosions that do not breach the sea surface consist of a series of pulses due to gas bubble oscillations. The period of oscillation is a well-known function of the yield and detonation depth for explosives up to several thousand kilograms of TNT equivalent. The presence of a bubble pulse is a strong indicator of an explosive source and, therefore, is useful in event characterization. Examples of underwater explosions, which can be used to calibrate signal processing algorithms and propagation models, are rare. A set of explosive and other impulsive events recorded on hydrophones at Wake Island and Point Sur, CA is presented. These include the French nuclear tests, volcanic events, and chemical explosions. The set also includes pressure time-series simulated using a normal-mode propagation model. The automatic signal processor has been developed to search the real cepstrum for peaks using a noise-spectral equalization algorithm similar to those used in passive sonar. Examples illustrate complications due to range, depth, ambient noise, and waveguide distortion.
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