Difference between revisions of "CVM-H"
| Line 29: | Line 29: | ||
=== Documentation === | === Documentation === | ||
| − | User Guide (includes installation instructions): [ | + | User Guide (includes installation instructions): [[CVM-H User Guide]] |
| Line 37: | Line 37: | ||
=== Development version === | === Development version === | ||
| − | If you're interested in working with the latest development version of the platform, you can check it out from | + | If you're interested in working with the latest development version of the platform, you can check it out from: |
svn co https://source.usc.edu/svn/cvmh/trunk | svn co https://source.usc.edu/svn/cvmh/trunk | ||
| Line 45: | Line 45: | ||
== Help == | == Help == | ||
| − | For assistance with the SCEC CVM-H, you may | + | For assistance with the SCEC CVM-H, you may: |
* Browse and submit new tickets at TBD | * Browse and submit new tickets at TBD | ||
* Email support @ scec.org with specific questions | * Email support @ scec.org with specific questions | ||
Revision as of 23:50, 10 January 2011
SCEC Community Velocity Model - Harvard (CVM-H)
Contents
Overview
The CVM-H is a velocity model of crust and upper mantle structure in southern California developed by the SCEC community for use in fault systems analysis, strong ground motion prediction, and earthquake hazards assessment. The model describes seismic P- and S-wave velocities and densities, and is comprised of basin structures embedded in tomographic and teleseismic crust and upper mantle models.
This latest release of the CVM-H (6.2) is an important milestone for SCEC, as it represents the integration of various model components, including fully 3D waveform tomographic results. The CVM-H 6.2 consists of basin structures defined using high-quality industry seismic reflection profiles and tens of thousands of direct velocity measurements from boreholes (Plesch et al., 2009; Süss and Shaw, 2003). The basin structures are also compatible with the locations and displacements of major faults represented in the SCEC Community Fault Model (CFM) (Plesch et al., 2007). These basin structures were used to develop travel time tomographic models of the crust (after Hauksson, 2000) extending to a depth of 35 km, and upper mantle teleseismic and surface wave models extending to a depth of 300 km (Prindle and Tanimoto, 2006). These various model components were integrated and used to perform a series of 3D adjoint tomographic inversions that highlight areas of the model that were responsible for mismatches between observed and synthetic waveforms (Tape et al, 2009). Sixteen tomographic iterations, requiring 6800 wavefield simulations, yielded perturbations to the starting model that have been incorporated in the latest model release. CVM-H 6.2 also incorporates a new Moho surface (Yan and Clayton, 2007) and a series of other upgrades to the geotechnical layer (GTL), the Vp-density scaling relationship, and the code that delivers the model.
Current Release
The current version of SCEC CVM-H is 11.1.0.
Dependencies
None.
Source code
SCEC CVM-H: [1]
md5sum: [2]
Documentation
User Guide (includes installation instructions): CVM-H User Guide
Supporting Materials
Development version
If you're interested in working with the latest development version of the platform, you can check it out from:
svn co https://source.usc.edu/svn/cvmh/trunk
Details about working with the development version are provided in the User Guide.
Help
For assistance with the SCEC CVM-H, you may:
- Browse and submit new tickets at TBD
- Email support @ scec.org with specific questions
License
This software is released under the following license agreement with provided disclaimers: TBD
Release History
11.1.0 - January 2011 - Initial release.
See Also
