Monochromatic body waves excited by great subduction zone earthquakes

Large quasi‐monochromatic body waves were excited by the 1995 Chile M w =8.1 and by the 1994 Kurile M w =8.3 events. They are observed on vertical/radial component seismograms following the direct P and P diff arrivals, at all azimuths. We devise a slant stack algorithm to characterize the source of the oscillations. This technique aims at locating near‐source isotropic scatterers using broadband data from global networks. For both events, we find that the oscillations emanate from the trench. We show that these monochromatic waves are due to localized oscillations of the water column. Their period corresponds to the gravest ID mode of a water layer for vertically traveling compressional waves. We suggest that these monochromatic body waves may yield additional constraints on the source process of great subduction zone earthquakes.