期刊
GEOPHYSICAL RESEARCH LETTERS
卷 42, 期 2, 页码 316-322出版社
AMER GEOPHYSICAL UNION
DOI: 10.1002/2014GL062347
关键词
microseismic noise; surface waves; tide modulation; secondary peak
资金
- PYROPE project [ANR-09-0229-000]
- VIBRIS project (Council of Pays de la Loire)
- Nantes-Atlantique Observatory (OSUNA)
- TopoIberia [CSD2006-00041, CGL2013-48601-C2-1-R]
Ocean activity produces continuous and ubiquitous seismic energy mostly in the 2-20 s period band, known as microseismic noise. Between 2and 10 s period, secondary microseisms (SM) are generated by swell reflections close to the shores and/or by opposing swells in the deep ocean. However, unique conditions are required in order for surface waves generated by deep-ocean microseisms to be observed on land. By comparing short-duration power spectral densities at both Atlantic shoreline and inland seismic stations, we show that ocean tides strongly modulate the seismic energy in a wide period band except between 2.5 and 5 s. This tidal proxy reveals the existence of an ex situ short-period contribution of the SM peak. Comparison with swell spectra at surrounding buoys suggests that the largest part of this extra energy comes from deep ocean-generated microseisms. The energy modulation might be also used in numerical models of microseismic generation to constrain coastal reflection coefficients.
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