Using Git for Team Collaboration
Tutorial on how to use Git and GitHub for team collaboration on a project. Content includes installing, setting up, creating a repository, making commits, un...
The Global Seismology Research Group resides at UC Berkeley, within the Department of Earth and Planetary Science and the Berkeley Seismological Laboratory.
Our research focuses on improving our understanding of the present day structure and internal dynamics of our planet, from the crust to the inner core, using seismic imaging approaches. We tackle the development and application of new methods for the computation of the seismic wavefield in complex 3D media, with a focus on complex structure in the deep mantle, and for tomographic imaging of elastic and anelastic structure using full waveform inversion (FWI), at the global and regional scale. For our applications, we make use HPC supercomputing facilities at NERSC and ACCESS. One of our recent interests is in the development and implementation of "Box Tomography", i.e. how to perform FWI of remote target regions in the deep earth at the short periods relevant to teleseismic observations, while keeping the computational cost manageable.
One of our more exotic research directions concerns the Earth's "hum" and the insights it brings to ocean/atmosphere/solid earth interactions. In order to better understand the chemical and thermal state of the mantle and the processes operating therein, we also seek to apply the latest findings of the mineral physics community within the context of our seismic probing and geodynamic modeling.
We also have an interest in the of study earthquake source mechanisms and scaling laws, as well as global seismic moment release and its relation to plate tectonics.
Our research is supported through a variety of sources, mostly through grants from NSF.
Tutorial on how to use Git and GitHub for team collaboration on a project. Content includes installing, setting up, creating a repository, making commits, un...
We implement the distributional finite difference method for 3D seismic wave propagation, which show promise for improving accuracy, flexibility, and efficie...
Progressive crystallisation of Earth’s inner core drives convection in the outer core and magnetic field generation. Determining the rate and pattern of inne...
Using a regional tomographic model of the Alaskan upper mantle to predict upper mantle effects on PKP travel times, we show that the signature of the Alaska ...
Based on the PKPdf observations and our new tomography model of the upper mantle beneath Alaska, we conclude that at least 2 s of the travel time anomaly oft...
Ultralow-velocity zones are localized regions of extreme material properties detected seismologically at the base of Earth’s mantle. Their nature and role in...
Explore seismic wave propagation using normal modes, NACT, and advanced theoretical models for global tomography.
Superplumes from the Core-Mantle Boundary to the Lithosphere: Implications for Heat Flux
Welcome to the online home of the SEMum2 model, a global radially anisotropic shear-velocity model of the earth’s upper mantle and transition zone.
Understanding the relationship between different scales of convection that drive plate motions and hotspot volcanism still eludes geophysicists. Using full-w...