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...
Published in: | Geophysical Journal of the Royal Astronomical Society |
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Oxford University Press
1973
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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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HighWire Press (Stanford University) |
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English |
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Articles |
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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 |
geographic_facet |
Yellowknife |
genre |
Yellowknife |
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 |
_version_ |
1766236755533496320 |