Regional P-Coda for Stable Estimates of Body Wave Magnitude: Extending the M(s):m(b) Discriminant to Smaller Events

The most successful teleseismic discriminant is M(s):m(b), and many studies are underway to try and extend surface wave magnitude (M(s)) estimation to regional distances. A problem that is encountered at regional distances and small magnitudes is how to estimate m(b) so that the M(s):m(b) discrimina...

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Main Authors: Mayeda, Kevin, Bonner, Jessie, Hooper, Heather
Other Authors: WESTON GEOPHYSICAL LEXINGTON MA
Format: Text
Language:English
Published: 2006
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA458608
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA458608
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spelling ftdtic:ADA458608 2023-05-15T17:47:15+02:00 Regional P-Coda for Stable Estimates of Body Wave Magnitude: Extending the M(s):m(b) Discriminant to Smaller Events Mayeda, Kevin Bonner, Jessie Hooper, Heather WESTON GEOPHYSICAL LEXINGTON MA 2006-09 text/html http://www.dtic.mil/docs/citations/ADA458608 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA458608 en eng http://www.dtic.mil/docs/citations/ADA458608 Approved for public release; distribution is unlimited. DTIC Nuclear Explosions and Devices(non-military) *NUCLEAR EXPLOSION TESTING *SEISMIC WAVES *ESTIMATES *DISCRIMINANT ANALYSIS WAVE PROPAGATION SURFACE WAVES SYMPOSIA METHODOLOGY SEISMIC CHARACTERIZATION SEISMIC PROPAGATION P-CODA METHODOLOGY COMPONENT REPORTS PE62601F WUAFRL1010SMA1 Text 2006 ftdtic 2016-02-23T02:23:11Z The most successful teleseismic discriminant is M(s):m(b), and many studies are underway to try and extend surface wave magnitude (M(s)) estimation to regional distances. A problem that is encountered at regional distances and small magnitudes is how to estimate m(b) so that the M(s):m(b) discriminant is meaningful and consistent with teleseismic measures. Over the past several years, a regional S-coda wave methodology has been developed that provides for the lowest variance estimate of the seismic source spectrum. Thus, regional M(w) and m(b) estimates derived from Sn and Lg coda are very stable, even when only a single station is used. However, these m(b)'s are inherently biased for earthquakes because they are an S-based measurement, and explosions are relatively depleted in S-waves. Previous research projects have used region-specific m(b) scales based on direct measurements of Pn and Pg to improve the M(s):m(b) discrimination, even though the m(b) estimates often had a large variance. The next obvious step to be implemented in the coda wave methodology is the use of P coda for m(b) estimates. This study focuses on developing a regional P-coda methodology to earthquakes and explosions on or near the Nevada, Shagan, Lop Nor, and Novaya Zemlya (NZ) test sites. Presented at the Symposium on Seismic Research (28th), Ground-based Nuclear Explosion Monitoring Technologies, held in Orlando, FL, on 19-21 Sep 2006. Published in the Seismic Research Review, v1 p625-635, 2006. The original document contains color images. Text Novaya Zemlya Defense Technical Information Center: DTIC Technical Reports database
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Nuclear Explosions and Devices(non-military)
*NUCLEAR EXPLOSION TESTING
*SEISMIC WAVES
*ESTIMATES
*DISCRIMINANT ANALYSIS
WAVE PROPAGATION
SURFACE WAVES
SYMPOSIA
METHODOLOGY
SEISMIC CHARACTERIZATION
SEISMIC PROPAGATION
P-CODA METHODOLOGY
COMPONENT REPORTS
PE62601F
WUAFRL1010SMA1
spellingShingle Nuclear Explosions and Devices(non-military)
*NUCLEAR EXPLOSION TESTING
*SEISMIC WAVES
*ESTIMATES
*DISCRIMINANT ANALYSIS
WAVE PROPAGATION
SURFACE WAVES
SYMPOSIA
METHODOLOGY
SEISMIC CHARACTERIZATION
SEISMIC PROPAGATION
P-CODA METHODOLOGY
COMPONENT REPORTS
PE62601F
WUAFRL1010SMA1
Mayeda, Kevin
Bonner, Jessie
Hooper, Heather
Regional P-Coda for Stable Estimates of Body Wave Magnitude: Extending the M(s):m(b) Discriminant to Smaller Events
topic_facet Nuclear Explosions and Devices(non-military)
*NUCLEAR EXPLOSION TESTING
*SEISMIC WAVES
*ESTIMATES
*DISCRIMINANT ANALYSIS
WAVE PROPAGATION
SURFACE WAVES
SYMPOSIA
METHODOLOGY
SEISMIC CHARACTERIZATION
SEISMIC PROPAGATION
P-CODA METHODOLOGY
COMPONENT REPORTS
PE62601F
WUAFRL1010SMA1
description The most successful teleseismic discriminant is M(s):m(b), and many studies are underway to try and extend surface wave magnitude (M(s)) estimation to regional distances. A problem that is encountered at regional distances and small magnitudes is how to estimate m(b) so that the M(s):m(b) discriminant is meaningful and consistent with teleseismic measures. Over the past several years, a regional S-coda wave methodology has been developed that provides for the lowest variance estimate of the seismic source spectrum. Thus, regional M(w) and m(b) estimates derived from Sn and Lg coda are very stable, even when only a single station is used. However, these m(b)'s are inherently biased for earthquakes because they are an S-based measurement, and explosions are relatively depleted in S-waves. Previous research projects have used region-specific m(b) scales based on direct measurements of Pn and Pg to improve the M(s):m(b) discrimination, even though the m(b) estimates often had a large variance. The next obvious step to be implemented in the coda wave methodology is the use of P coda for m(b) estimates. This study focuses on developing a regional P-coda methodology to earthquakes and explosions on or near the Nevada, Shagan, Lop Nor, and Novaya Zemlya (NZ) test sites. Presented at the Symposium on Seismic Research (28th), Ground-based Nuclear Explosion Monitoring Technologies, held in Orlando, FL, on 19-21 Sep 2006. Published in the Seismic Research Review, v1 p625-635, 2006. The original document contains color images.
author2 WESTON GEOPHYSICAL LEXINGTON MA
format Text
author Mayeda, Kevin
Bonner, Jessie
Hooper, Heather
author_facet Mayeda, Kevin
Bonner, Jessie
Hooper, Heather
author_sort Mayeda, Kevin
title Regional P-Coda for Stable Estimates of Body Wave Magnitude: Extending the M(s):m(b) Discriminant to Smaller Events
title_short Regional P-Coda for Stable Estimates of Body Wave Magnitude: Extending the M(s):m(b) Discriminant to Smaller Events
title_full Regional P-Coda for Stable Estimates of Body Wave Magnitude: Extending the M(s):m(b) Discriminant to Smaller Events
title_fullStr Regional P-Coda for Stable Estimates of Body Wave Magnitude: Extending the M(s):m(b) Discriminant to Smaller Events
title_full_unstemmed Regional P-Coda for Stable Estimates of Body Wave Magnitude: Extending the M(s):m(b) Discriminant to Smaller Events
title_sort regional p-coda for stable estimates of body wave magnitude: extending the m(s):m(b) discriminant to smaller events
publishDate 2006
url http://www.dtic.mil/docs/citations/ADA458608
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA458608
genre Novaya Zemlya
genre_facet Novaya Zemlya
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA458608
op_rights Approved for public release; distribution is unlimited.
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