Global P, PP, and PKP wave microseisms observed from distant storms

By Peter Gerstoft, P. Shearer, N. Harmon, Jian Zhang. 2008

180 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

Shear wave imaging from traffic noise using seismic interferometry by cross-coherence (2011, methodology): “We pick the phase velocity of the fundamental mode Love wave (blue crosses in Figure 5c) and use thesemeasurements to invert for the shear-velocity as a function of depth using a genetic algorithm (Saito and Kabasawa, 1993; Yamanaka and Ishida, 1995; Hayashi, 2008).”
Origin of deep ocean microseisms by using teleseismic body waves (2010, background): “…were detected in the secondary microseismic band using dense seismic arrays [e.g., Backus et al., 1964; Toksöz and Lacoss, 1968; Seriff et al., 1965; Iyer and Healy, 1972; Koper and de Foy, 2008; Gerstoft et al., 2008] and can be often associated with specific storms [e.g., Gerstoft et al., 2006].”
Retrieval of Moho‐reflected shear wave arrivals from ambient seismic noise (2010, unknown): “The NCFs of the summer seasons are not used here because the strong teleseismic Pwave energy from storms in the southern hemisphere causes strong artefacts near zero lag time (Gerstoft et al. 2008).”