Los Alamos Seismic Network EES-17 SS Team Challenge: Identify Odd LASN Events [Slides]
An overview of local earthquake signals is provided, and the team's signals recorded are shown.
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An overview of local earthquake signals is provided, and the team's signals recorded are shown.
The report details a series of software tools and workflows to analyze surface deformation data obtained from InSAR, deformation evidence by earthquake, geological constraints, and reservoir management to define and monitor the geothermal reservoir.
Goals for the project included: Testing the limits of RSTT resolving capability; Increasing accuracy of travel time predictions (used for earthquake location) through data-dictated grid refinement; and, refining subsurface images of Israel and the Eastern Mediterranean and tectonic structures in the area.
The Geophysical Monitoring Program (GMP) at Lawrence Livermore National Lab (LLNL) maintains a database and supporting infrastructure for geophysical data used in support of the Nuclear Detonation Detection mission. This database includes data from multiple sources, many of which do not distribute data to the public or for which there is no automated means of access. For example, Figure 1 shows (left) the distribution of waveform data in our database by source. The Incorporated Research Institutions for Seismology Data Management Center (IRISDMC) is our major source of waveform data and those data may be retrieved at will using the Federated Digital Seismograph Networks FDSN web Application Programming Interface (API). However, the next 6 most important sources of waveform data have no or only limited automated access to waveforms. As Figure 1 (right) shows, it is very common for waveform records associate with an event in our database to come from two or more sources, and in some cases data come from 10 sources. This diversity of data sources drives our need for efficient and correct integration of metadata, parametric data, and waveform data.
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