Mid-ocean microseisms

Author:

Bromirski Peter D.1,Duennebier Fred K.2,Stephen Ralph A.3

Affiliation:

1. Integrative Oceanography Division, Scripps Institution of Oceanography; University of California, San Diego; 9500 Gilman Drive,; La Jolla; California; 92093-0209; USA

2. Department of Geology and Geophysics, School of Ocean and Earth Sciences and Technology; University of Hawaii; Honolulu; Hawaii; 96822; USA

3. Woods Hole Oceanographic Institution; Woods Hole; Massachusetts; 02543-1542; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference28 articles.

1. Relationship between ocean bottom noise and the environment;Babcock;Bull. Seismol. Soc. Am.,1994

2. Very low frequency (0.2-10.0 Hz) seismoacoustic noise below the seafloor;Bradley;J. Geophys. Res.,1997

3. Vibrations from the “Perfect Storm,”;Bromirski;Geochem. Geophys. Geosyst.,2001

4. The near-coastal microseism spectrum: Spatial and temporal wave climate relationships;Bromirski;J. Geophys. Res.,2002

5. Ocean wave height determined from inland seismometer data: Implications for investigating wave climate changes in the NE Pacific;Bromirski;J. Geophys. Res.,1999

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