Multidecadal Climate-induced Variability in Microseisms

Research Article| March 01, 2008 Multidecadal Climate-induced Variability in Microseisms Richard C. Aster; Richard C. Aster Department of Earth and Environmental Science Geophysical Research Center New Mexico Institute of Mining and Technology Socorro, New Mexico 87801 USA aster@ees.nmt.edu (R.A.) Search for other works by this author on: GSW Google Scholar Daniel E. McNamara; Daniel E. McNamara U.S. Geological Survey 1711 Illinois St. Golden, Colorado 80401 USA mcnamara@usgs.gov (D.M.) Search for other works by this author on: GSW Google Scholar Peter D. Bromirski Peter D. Bromirski Scripps Institution of Oceanography Integrative Oceanography Division 0209 9500 Gilman Drive Scripps Institution of Oceanography La Jolla, California 92093-0209 USA pbromirski@ucsd.edu (P.B.) Search for other works by this author on: GSW Google Scholar Author and Article Information Richard C. Aster Department of Earth and Environmental Science Geophysical Research Center New Mexico Institute of Mining and Technology Socorro, New Mexico 87801 USA aster@ees.nmt.edu (R.A.) Daniel E. McNamara U.S. Geological Survey 1711 Illinois St. Golden, Colorado 80401 USA mcnamara@usgs.gov (D.M.) Peter D. Bromirski Scripps Institution of Oceanography Integrative Oceanography Division 0209 9500 Gilman Drive Scripps Institution of Oceanography La Jolla, California 92093-0209 USA pbromirski@ucsd.edu (P.B.) Publisher: Seismological Society of America First Online: 09 Mar 2017 Online ISSN: 1938-2057 Print ISSN: 0895-0695 © 2008 by the Seismological Society of America Seismological Research Letters (2008) 79 (2): 194–202. https://doi.org/10.1785/gssrl.79.2.194 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Richard C. Aster, Daniel E. McNamara, Peter D. Bromirski; Multidecadal Climate-induced Variability in Microseisms. Seismological Research Letters 2008;; 79 (2): 194–202. doi: https://doi.org/10.1785/gssrl.79.2.194 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search Microseisms are the most ubiquitous continuous seismic signals on Earth at periods between approximately 5 and 25 s (Peterson 1993; Kedar and Webb 2005). They arise from atmospheric energy converted to (primarily) Rayleigh waves via the intermediary of wind-driven oceanic swell and occupy a period band that is uninfluenced by common anthropogenic and wind-coupled noise processes on land (Wilson et al. 2002; de la Torre et al. 2005). "Primary" microseisms (near 8-s period) are generated in shallow water by breaking waves near the shore and/or the nonlinear interaction of the ocean wave pressure signal with... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.