The origin of deep ocean microseisms in the North Atlantic Ocean

By S. Kedar, M. Longuet-Higgins, F. Webb, N. Graham, Robert W. Clayton, Cathleen E. Jones. Proceedings of the Royal Society A, 2007

306 citations recorded by the source corpus.

Subfields: Geophysics

View Paper: https://www.semanticscholar.org/paper/caec25425dd65f0b128cdec4be46b89b9b0eee6f

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Citations in the corpus

Global climate imprint on seismic noise (2009, background): “Recently, modeling of the deep ocean nonlinear wave-wave interaction in a source region between the Labrador Sea and Iceland showed an excellent agreement with the secondary microseism amplitude recorded by stations in North America and Western Europe [Kedar et al., 2007], demonstrating the validity”
Global P, PP, and PKP wave microseisms observed from distant storms (2008, background): “interaction maps [Kedar et al., 2008], if available, might provide a more relevant comparison.”
On establishing the accuracy of noise tomography travel‐time measurements in a realistic medium (2009, background): “Snieder 2004; Kedar et al. 2008 ); scattering of seismic energy is thought to be more efficient in the near-surface heterogeneous lithosphere (e.g.”
Geophysics From Terrestrial Time‐Variable Gravity Measurements (2017, background): “Even in the absence of an earthquake, the displacements of the Earth’s surface are persistent and location and season dependent, reaching up to a few micrometers close to the coast (Kedar et al., 2008), while one should measure the free-fall distance at the 1 nm”
How ocean waves rock the Earth: Two mechanisms explain microseisms with periods 3 to 300 s (2015, background): “Here we focus on vertical motions which are dominated by Rayleigh waves, but horizontal motions corresponding to Love waves can also be very energetic [Kurrle and Widmer-Schnidrig, 2008].”
A global wave parameter database for geophysical applications. Part 1: Wave-current turbulence interaction parameters for the open ocean based on traditional parameterizations (2008, methodology): “These include parameters relevant for remote sensing applications, momentum fluxes in and out of the wave field to allow a modelling of the full wave-current coupling (Ardhuin et al., 2008c), and microseism generation forces (e.g., Kedar et al., 2008).”
Monitoring and analysis of ocean swell fields from space: New methods for routine observations (2009, background): “Yet this question if of high practical importance, either for wave forecasting [e.g., Rascle et al., 2008] or other geophysical investigations regarding air-sea fluxes or microseismic noise [e.g., Grachev and Fairall, 2001; Kedar et al., 2008].”
Origin of deep ocean microseisms by using teleseismic body waves (2010, background): “, 2004; Rhie and Romanowicz, 2006; Yang and Ritzwoller, 2008] or if it is also generated in deep‐sea areas [Cessaro, 1994; Stehly et al., 2006; Chevrot et al., 2007; Kedar et al., 2008].”
Ocean wave sources of seismic noise (2011, unknown): “The only similar previous model, by Kedar et al. [2008], did not include coastal reflections and thus could not reproduce some of the recorded noise events.”
Reconstructing Green's function by correlation of the coda of the correlation (C3) of ambient seismic noise (2008, background): “As a matter of fact the noise in our region of study is dominated by the contribution of sources in the North Atlantic [e.g., Stehly et al., 2006; Kedar et al., 2008].”