Propagation of microseisms from the deep ocean to land
|Title:||Propagation of microseisms from the deep ocean to land||Authors:||Ying, Yingzi
Bean, Christopher J.
Bromirski, Peter D.
|Permanent link:||http://hdl.handle.net/10197/6119||Date:||22-Sep-2014||Abstract:||Ocean-generated microseisms are faint Earth vibrations that result from pressure fluctuations at the sea floor generated by the interaction between ocean surface gravity waves, and are continuously recorded as low frequency seismic noise. Here we investigate microseism propagation away from deep-ocean source regions using the spectral element method for an oceanic model that contains realistic northeast Atlantic Ocean irregular-layered structure composed of water, sediment, and upper crust. It also includes structural heterogeneities and continental slope and shelf bathymetry. Numerical simulations of coupled acoustic and elastic wave propagation in both simplified models and the full realistic model show that most microseism energy is confined to sediment and water column waveguides. We also show that a significant portion of microseism energy is reflected back to the deep ocean by the continental slope, while only a small fraction of deep-ocean-generated microseism energy reaches land. We conclude that terrestrially observed microseisms are largely generated in shallow water on continental shelves.||Funding Details:||Science Foundation Ireland||Type of material:||Journal Article||Publisher:||AIP Publishing||Journal:||Geophysical Research Letters||Volume:||41||Issue:||18||Start page:||6374||End page:||6379||Copyright (published version):||2014 American Geophysical Union||Keywords:||Computational seismology; Wave propagation; Fluid-solid coupling; Secondary microseism||DOI:||10.1002/2014GL060979||Language:||en||Status of Item:||Peer reviewed||metadata.dc.date.available:||2015-03-22T04:00:22Z|
|Appears in Collections:||Earth Sciences Research Collection|
Show full item record
This item is available under the Attribution-NonCommercial-NoDerivs 3.0 Ireland. No item may be reproduced for commercial purposes. For other possible restrictions on use please refer to the publisher's URL where this is made available, or to notes contained in the item itself. Other terms may apply.