Advanced Regional Array Studies

We have addressed the problem of optimizing the site-specific seismic threshold monitoring method in order to achieve the highest possible automatic monitoring capability of particularly interesting areas, such as the Novaya Zemlya testing area, and the Indian and Pakistani test sites. For the Novay...

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Main Author: Kvaerna, Tormod
Other Authors: NORWEGIAN SEISMIC ARRAY (NORSAR) KJELLER
Format: Text
Language:English
Published: 2001
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA400396
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA400396
id ftdtic:ADA400396
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spelling ftdtic:ADA400396 2023-05-15T17:47:13+02:00 Advanced Regional Array Studies Kvaerna, Tormod NORWEGIAN SEISMIC ARRAY (NORSAR) KJELLER 2001-09 text/html http://www.dtic.mil/docs/citations/ADA400396 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA400396 en eng http://www.dtic.mil/docs/citations/ADA400396 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Seismology *SEISMOLOGY SIGNAL PROCESSING FREQUENCY NUCLEAR EXPLOSIONS SURFACE WAVES DATA TRANSMISSION SYSTEMS MONITORING NETWORKS SEISMIC DETECTION SEISMIC WAVES AMPLIFICATION NORWAY SEISMIC ARRAYS FOREIGN REPORTS Text 2001 ftdtic 2016-02-20T15:05:55Z We have addressed the problem of optimizing the site-specific seismic threshold monitoring method in order to achieve the highest possible automatic monitoring capability of particularly interesting areas, such as the Novaya Zemlya testing area, and the Indian and Pakistani test sites. For the Novaya Zemlya test site, where a regional monitoring network is available, we obtain a monitoring capability varying between m(sub b) 2.0 and 2.5 during normal noise conditions. Based on data from the teleseismic network observing the Indian and Pakistani tests of 1998, we obtain a monitoring capability in the range m(sub b) 2.8-3.0 for these test sites. In order to fully automate the site-specific threshold monitoring method, we have developed an automatic explanation facility for analysis of the threshold traces. In this way threshold peaks caused by events located outside the target region can be discarded from further analysis. We have also extended the site-specific threshold monitoring method to process surface waves. An important results of this study is the demonstration of the significant benefits of using a shorter period band (8.12 seconds) instead of the traditional processing band (17-24 seconds) for processing surface waves at regional disturbances during an aftershock sequence. --Original contains color plates: All DTIC reproductions will be in black and white. Text Novaya Zemlya Defense Technical Information Center: DTIC Technical Reports database Indian Norway
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Seismology
*SEISMOLOGY
SIGNAL PROCESSING
FREQUENCY
NUCLEAR EXPLOSIONS
SURFACE WAVES
DATA TRANSMISSION SYSTEMS
MONITORING
NETWORKS
SEISMIC DETECTION
SEISMIC WAVES
AMPLIFICATION
NORWAY
SEISMIC ARRAYS
FOREIGN REPORTS
spellingShingle Seismology
*SEISMOLOGY
SIGNAL PROCESSING
FREQUENCY
NUCLEAR EXPLOSIONS
SURFACE WAVES
DATA TRANSMISSION SYSTEMS
MONITORING
NETWORKS
SEISMIC DETECTION
SEISMIC WAVES
AMPLIFICATION
NORWAY
SEISMIC ARRAYS
FOREIGN REPORTS
Kvaerna, Tormod
Advanced Regional Array Studies
topic_facet Seismology
*SEISMOLOGY
SIGNAL PROCESSING
FREQUENCY
NUCLEAR EXPLOSIONS
SURFACE WAVES
DATA TRANSMISSION SYSTEMS
MONITORING
NETWORKS
SEISMIC DETECTION
SEISMIC WAVES
AMPLIFICATION
NORWAY
SEISMIC ARRAYS
FOREIGN REPORTS
description We have addressed the problem of optimizing the site-specific seismic threshold monitoring method in order to achieve the highest possible automatic monitoring capability of particularly interesting areas, such as the Novaya Zemlya testing area, and the Indian and Pakistani test sites. For the Novaya Zemlya test site, where a regional monitoring network is available, we obtain a monitoring capability varying between m(sub b) 2.0 and 2.5 during normal noise conditions. Based on data from the teleseismic network observing the Indian and Pakistani tests of 1998, we obtain a monitoring capability in the range m(sub b) 2.8-3.0 for these test sites. In order to fully automate the site-specific threshold monitoring method, we have developed an automatic explanation facility for analysis of the threshold traces. In this way threshold peaks caused by events located outside the target region can be discarded from further analysis. We have also extended the site-specific threshold monitoring method to process surface waves. An important results of this study is the demonstration of the significant benefits of using a shorter period band (8.12 seconds) instead of the traditional processing band (17-24 seconds) for processing surface waves at regional disturbances during an aftershock sequence. --Original contains color plates: All DTIC reproductions will be in black and white.
author2 NORWEGIAN SEISMIC ARRAY (NORSAR) KJELLER
format Text
author Kvaerna, Tormod
author_facet Kvaerna, Tormod
author_sort Kvaerna, Tormod
title Advanced Regional Array Studies
title_short Advanced Regional Array Studies
title_full Advanced Regional Array Studies
title_fullStr Advanced Regional Array Studies
title_full_unstemmed Advanced Regional Array Studies
title_sort advanced regional array studies
publishDate 2001
url http://www.dtic.mil/docs/citations/ADA400396
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA400396
geographic Indian
Norway
geographic_facet Indian
Norway
genre Novaya Zemlya
genre_facet Novaya Zemlya
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA400396
op_rights APPROVED FOR PUBLIC RELEASE
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