Open AccessMicroseisms and hum from ocean surface gravity waves
Author(s) -
Traer James,
Gerstoft Peter,
Bromirski Peter D.,
Shearer Peter M.
Publication year - 2012
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2012jb009550
Subject(s) - microseism , geology , seismology , infragravity wave , swell , wind wave , rayleigh wave , storm , hum , geophysics , azimuth , surface wave , love wave , oceanography , wave propagation , longitudinal wave , mechanical wave , physics , art , quantum mechanics , astronomy , performance art , art history
Ocean waves incident on coasts generate seismic surface waves in three frequency bands via three pathways: direct pressure on the seafloor (primary microseisms, PM), standing waves from interaction of incident and reflected waves (double‐frequency microseisms, DF), and swell‐transformed infragravity wave interactions (the Earth's seismic hum). Beamforming of USArray seismic data shows that the source azimuths of the generation regions of hum, PM and DF microseisms vary seasonally, consistent with hemispheric storm patterns. The correlation of beam power with wave height over all azimuths is highest in near‐coastal waters. Seismic signals generated by waves from Hurricane Irene and from a storm in the Southern Ocean have good spatial and temporal correlation with nearshore wave height and peak period for all three wave‐induced seismic signals, suggesting that ocean waves in shallow water commonly excite hum (via infragravity waves), PM, and DF microseisms concurrently.