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Titlebook: Earthquake Monitoring and Seismic Hazard Mitigation in Balkan Countries; Eystein S. Husebye Conference proceedings 2008 Springer Science+B

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The CTBTO International Monitoring System and Global Seismicitythe policy-making organs of the PrepCom plenary body in conjunction with three working and advisory groups and the Provisional Technical Secretariat (PTS). The PTS started its work in Vienna, Austria in March 1997 and consists, besides administrative and legal divisions, of three technical divisions
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The IRIS Consortium: Community Based Facilities and Data Management for Seismologynwavering commitment to free and unrestricted data availability have stimulated profound changes in attitudes among Earth scientists that strongly discourage proprietary data. These attitudes underlay a new era of discoveries about the Earth and explosive growth in Earth science information, includi
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GEOFON and its Role in Earthquake Monitoring and Tsunami Warningrly Warning System (GITEWS). Beside the earthquake monitoring and the operation of a major global seismic broadband network GEOFON runs the largest seismological data archive in Europe. In addition, the cooperation and networking of European and other data centers both in terms of real-time data exc
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Cossack Ranger II – A High Quality, Versatile and Affordable 3-Component Short-Period Seismographugh an outreach project named SeiSchool aimed at cooperation with local high schools. The latter have permanent access to the Internet so data transfer to the Hub in Institute was free. Some schools even installed their own seismographs locally with only written instructions at hand. Station operati
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Accurate Location of Seismic Sources With and Without Travel Time Modelhich are tied to bulletin phase pickings at different stations for a given event. The final location solution is the maximum of the location probability density function (PDF) and 90% confidence volume, determined by the grid-based PDF distribution. The PDF location is shown to be a convolution betw
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Earthworm Auto-Earthquake Location Performance and Recent Improvements in Seismic Data Acquisition, reshold for a 90% earthquake auto-detection and location reliability. For the rest of the country this low magnitude threshold estimate ranges between 4.4 and 4.6. Three initiatives have been proposed to improve EW auto-detection and location accuracy. These are more accurate timing of emergent phas
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