An Attempt to Detect Gravitational Waves with the Yellowknife Seismic Array

The Yellowknife array of 19 vertical short-period seismometers was used to search for small coherent signals in the frequency range from about 1 to 8 Hz. Beamforming and autocorrelation of several hours of digital seismic recording lowers the background noise level to about 10−11 ms−1. Consistent pe...

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Published in:Geophysical Journal of the Royal Astronomical Society
Main Author: Weichert, D. H.
Format: Text
Language:English
Published: Oxford University Press 1973
Subjects:
Online Access:http://gji.oxfordjournals.org/cgi/content/short/35/1-3/337
https://doi.org/10.1111/j.1365-246X.1973.tb02432.x
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spelling fthighwire:oai:open-archive.highwire.org:gji:35/1-3/337 2023-05-15T18:45:39+02:00 An Attempt to Detect Gravitational Waves with the Yellowknife Seismic Array Weichert, D. H. 1973-12-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/35/1-3/337 https://doi.org/10.1111/j.1365-246X.1973.tb02432.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/35/1-3/337 http://dx.doi.org/10.1111/j.1365-246X.1973.tb02432.x Copyright (C) 1973, Oxford University Press Articles TEXT 1973 fthighwire https://doi.org/10.1111/j.1365-246X.1973.tb02432.x 2016-11-16T19:00:58Z The Yellowknife array of 19 vertical short-period seismometers was used to search for small coherent signals in the frequency range from about 1 to 8 Hz. Beamforming and autocorrelation of several hours of digital seismic recording lowers the background noise level to about 10−11 ms−1. Consistent peaks are observed at several frequencies, but terrestrial or instrumental origins have been identified for most components. None of the observed components shows correlation with sidereal time. There is, therefore, no evidence that gravitational waves have been detected. Text Yellowknife HighWire Press (Stanford University) Yellowknife Geophysical Journal of the Royal Astronomical Society 35 1-3 337 342
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collection HighWire Press (Stanford University)
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language English
topic Articles
spellingShingle Articles
Weichert, D. H.
An Attempt to Detect Gravitational Waves with the Yellowknife Seismic Array
topic_facet Articles
description The Yellowknife array of 19 vertical short-period seismometers was used to search for small coherent signals in the frequency range from about 1 to 8 Hz. Beamforming and autocorrelation of several hours of digital seismic recording lowers the background noise level to about 10−11 ms−1. Consistent peaks are observed at several frequencies, but terrestrial or instrumental origins have been identified for most components. None of the observed components shows correlation with sidereal time. There is, therefore, no evidence that gravitational waves have been detected.
format Text
author Weichert, D. H.
author_facet Weichert, D. H.
author_sort Weichert, D. H.
title An Attempt to Detect Gravitational Waves with the Yellowknife Seismic Array
title_short An Attempt to Detect Gravitational Waves with the Yellowknife Seismic Array
title_full An Attempt to Detect Gravitational Waves with the Yellowknife Seismic Array
title_fullStr An Attempt to Detect Gravitational Waves with the Yellowknife Seismic Array
title_full_unstemmed An Attempt to Detect Gravitational Waves with the Yellowknife Seismic Array
title_sort attempt to detect gravitational waves with the yellowknife seismic array
publisher Oxford University Press
publishDate 1973
url http://gji.oxfordjournals.org/cgi/content/short/35/1-3/337
https://doi.org/10.1111/j.1365-246X.1973.tb02432.x
geographic Yellowknife
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genre_facet Yellowknife
op_relation http://gji.oxfordjournals.org/cgi/content/short/35/1-3/337
http://dx.doi.org/10.1111/j.1365-246X.1973.tb02432.x
op_rights Copyright (C) 1973, Oxford University Press
op_doi https://doi.org/10.1111/j.1365-246X.1973.tb02432.x
container_title Geophysical Journal of the Royal Astronomical Society
container_volume 35
container_issue 1-3
container_start_page 337
op_container_end_page 342
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