Index for 2aUW

• 2aUW1. The earthquake T phase: MILS hydrophone array results.
• 2aUW2. Monitoring microseismicity in the northeast Pacific using hydroacoustic techniques.
• 2aUW3. T-wave source level and earthquake fault parameters: Empirically derived scaling relationships.
• 2aUW4. A multipath model for T-wave generation by seafloor earthquakes.
• 2aUW5. Periodic deep-sea hydrothermal vent activities observed by hydrophones at Mariana, Okinawa, and Mid-Atlantic Ridge.
• 2aUW6. Seismic structure using body wave arrivals at SOSUS hydrophone arrays.
• 2aUW7. T-wave detection of underwater volcanism by land-based seismic stations: The example of the Hollister Ridge, Southern Pacific.
• 2aUW8. Arctic abyssal T-phase coupling to the ocean acoustic channel.
• 2aUW9. Acoustic array observations of seismic events.
• 2aUW10. Monitoring ocean seismicity using autonomous hydrophone moorings.
• 2aUW11. Modeling oceanic T-phase generation using coupled wave-number-integration approaches.
• 2aUW12. Possible mechanisms for T-phase generation.
• 2aUW13. An elastic wave diffusion theory for ocean crustal phase coda development.
• 2aUW14. Acoustic T-phase directionality measuments using a towed line array.
• 2aUW15. An automated system for detecting and classifying in-water explosions and T-phases.
• 2aUW16. A global monitoring system for a nuclear test ban treaty.
• 2aUW17. Doubly asymptotic approximations for transient elastodynamics.
• 2aUW18. Trapping of hydroacoustic waves generated by underwater earthquakes into a sound channel.