An investigation of analysis of variance as a tool for exploring regional differences in strong ground motions

The statistical technique known as analysis of variance is applied to a large set of European strong-motion data to investigate whether strong ground motions show a regional dependence. This question is important when selecting strong-motion records for the derivation of ground motion prediction equ...

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Published in:Journal of Seismology
Main Author: Douglas, John
Format: Article in Journal/Newspaper
Language:unknown
Published: 2004
Subjects:
Online Access:https://strathprints.strath.ac.uk/53448/
https://doi.org/10.1007/s10950-004-3094-7
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spelling ftustrathclyde:oai:strathprints.strath.ac.uk:53448 2024-04-28T08:26:01+00:00 An investigation of analysis of variance as a tool for exploring regional differences in strong ground motions Douglas, John 2004-10-01 https://strathprints.strath.ac.uk/53448/ https://doi.org/10.1007/s10950-004-3094-7 unknown Douglas, John <https://strathprints.strath.ac.uk/view/author/1027421.html> (2004 <https://strathprints.strath.ac.uk/view/year/2004.html>) An investigation of analysis of variance as a tool for exploring regional differences in strong ground motions. Journal of Seismology <https://strathprints.strath.ac.uk/view/publications/Journal_of_Seismology.html>, 8 (4). pp. 485-496. ISSN 1573-157X Engineering (General). Civil engineering (General) Article PeerReviewed 2004 ftustrathclyde https://doi.org/10.1007/s10950-004-3094-7 2024-04-10T01:04:04Z The statistical technique known as analysis of variance is applied to a large set of European strong-motion data to investigate whether strong ground motions show a regional dependence. This question is important when selecting strong-motion records for the derivation of ground motion prediction equations and also when choosing strong-motion records from one geographical region for design purposes in another. Five regions with much strong-motion data (the Caucasus region, central Italy, Friuli, Greece and south Iceland) are investigated here. For the magnitude and distance range where there are overlapping data from the five areas (2.50≤Ms≤5.50, 0≤d≤35 km) and consequently analysis of variance can be performed, there is little evidence for a regional dependence of ground motions. There is a lack of data from moderate and large magnitude earthquakes (Ms > 5.5) so analysis of variance cannot be performed there. Since there is uncertainty regarding scaling ground motions from small to large magnitudes whether ground motions from large earthquakes are significantly different in different parts of Europe is not known. Analysis of variance has the ability to complement other techniques for the assessment of regional dependence of ground motions. Article in Journal/Newspaper Iceland University of Strathclyde Glasgow: Strathprints Journal of Seismology 8 4 485 496
institution Open Polar
collection University of Strathclyde Glasgow: Strathprints
op_collection_id ftustrathclyde
language unknown
topic Engineering (General). Civil engineering (General)
spellingShingle Engineering (General). Civil engineering (General)
Douglas, John
An investigation of analysis of variance as a tool for exploring regional differences in strong ground motions
topic_facet Engineering (General). Civil engineering (General)
description The statistical technique known as analysis of variance is applied to a large set of European strong-motion data to investigate whether strong ground motions show a regional dependence. This question is important when selecting strong-motion records for the derivation of ground motion prediction equations and also when choosing strong-motion records from one geographical region for design purposes in another. Five regions with much strong-motion data (the Caucasus region, central Italy, Friuli, Greece and south Iceland) are investigated here. For the magnitude and distance range where there are overlapping data from the five areas (2.50≤Ms≤5.50, 0≤d≤35 km) and consequently analysis of variance can be performed, there is little evidence for a regional dependence of ground motions. There is a lack of data from moderate and large magnitude earthquakes (Ms > 5.5) so analysis of variance cannot be performed there. Since there is uncertainty regarding scaling ground motions from small to large magnitudes whether ground motions from large earthquakes are significantly different in different parts of Europe is not known. Analysis of variance has the ability to complement other techniques for the assessment of regional dependence of ground motions.
format Article in Journal/Newspaper
author Douglas, John
author_facet Douglas, John
author_sort Douglas, John
title An investigation of analysis of variance as a tool for exploring regional differences in strong ground motions
title_short An investigation of analysis of variance as a tool for exploring regional differences in strong ground motions
title_full An investigation of analysis of variance as a tool for exploring regional differences in strong ground motions
title_fullStr An investigation of analysis of variance as a tool for exploring regional differences in strong ground motions
title_full_unstemmed An investigation of analysis of variance as a tool for exploring regional differences in strong ground motions
title_sort investigation of analysis of variance as a tool for exploring regional differences in strong ground motions
publishDate 2004
url https://strathprints.strath.ac.uk/53448/
https://doi.org/10.1007/s10950-004-3094-7
genre Iceland
genre_facet Iceland
op_relation Douglas, John <https://strathprints.strath.ac.uk/view/author/1027421.html> (2004 <https://strathprints.strath.ac.uk/view/year/2004.html>) An investigation of analysis of variance as a tool for exploring regional differences in strong ground motions. Journal of Seismology <https://strathprints.strath.ac.uk/view/publications/Journal_of_Seismology.html>, 8 (4). pp. 485-496. ISSN 1573-157X
op_doi https://doi.org/10.1007/s10950-004-3094-7
container_title Journal of Seismology
container_volume 8
container_issue 4
container_start_page 485
op_container_end_page 496
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