Global seismographic networks (GSNs) emerged during the late nineteenth and early
twentieth centuries, facilitated by seminal international developments in theory, technology …

Earth's body tide—also known as the solid Earth tide, the displacement of the solid Earth's
surface caused by gravitational forces from the Moon and the Sun—is sensitive to the …

A large data set of surface wave phase anomalies, body wave travel times, normal‐mode
splitting functions, and long‐period waveforms is used to investigate the scaling between …

Abstract The Global Seismographic Network (GSN)—a global network of≈ 150 very
broadband stations—is used by researchers to study the free oscillations of the Earth (≈ 0.3 …

The dynamic topography of the core‐mantle boundary (CMB) provides important constraints
on dynamic processes in the mantle and core. However, inferences on CMB topography are …

Seismic free oscillations, or normal modes, provide a convenient tool to calculate low-
frequency seismograms in heterogeneous Earth models. A procedure called 'full mode …

Stoneley modes are a special subset of normal modes whose energy is confined along the
core–mantle boundary (CMB). As such, they offer a unique glimpse into Earth structure at …

The computational cost of full waveform simulation in seismological contexts is known to be
expensive and generally requires large clusters of computers working in parallel. Although …

Mantle flow induces dynamic topography at the core–mantle boundary (CMB), with
distribution and amplitude that depend on details of the flow. To assess whether …

Normal-mode spectra may be used to investigate large-scale elastic and anelastic
heterogeneity throughout the entire Earth. The relevant theory was developed a few …