On the Lateral Refraction of Rayleigh Surface Waves and Microseisms in the North Atlantic

The lateral refraction of microseisms with T = 6 s and of surface waves with T = 20 s has been computed for North Atlantic sources recorded at European stations (Pulkovo, Simferopol, Prague). Such surface waves are not always recorded at certain stations for all source regions owing to the peculiari...

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Published in:Geophysical Journal International
Main Authors: Savarensky, E. F., Proskuryakova, T. A., Glasko, V. B., Granit, Y. Sh., Voronina, E. V.
Format: Text
Language:English
Published: Oxford University Press 1968
Subjects:
Articles
North Atlantic
Online Access:http://gji.oxfordjournals.org/cgi/content/short/15/5/529
https://doi.org/10.1111/j.1365-246X.1968.tb00207.x
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spelling fthighwire:oai:open-archive.highwire.org:gji:15/5/529 2023-05-15T17:25:39+02:00 On the Lateral Refraction of Rayleigh Surface Waves and Microseisms in the North Atlantic Savarensky, E. F. Proskuryakova, T. A. Glasko, V. B. Granit, Y. Sh. Voronina, E. V. 1968-08-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/15/5/529 https://doi.org/10.1111/j.1365-246X.1968.tb00207.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/15/5/529 http://dx.doi.org/10.1111/j.1365-246X.1968.tb00207.x Copyright (C) 1968, Oxford University Press Articles TEXT 1968 fthighwire https://doi.org/10.1111/j.1365-246X.1968.tb00207.x 2015-02-28T18:55:16Z The lateral refraction of microseisms with T = 6 s and of surface waves with T = 20 s has been computed for North Atlantic sources recorded at European stations (Pulkovo, Simferopol, Prague). Such surface waves are not always recorded at certain stations for all source regions owing to the peculiarities of wave propagation. These pecularities should be taken into account when tracing the sources of North Atlantic microseisms. Text North Atlantic HighWire Press (Stanford University) Geophysical Journal International 15 5 529 544
institution Open Polar
collection HighWire Press (Stanford University)
op_collection_id fthighwire
language English
topic Articles
spellingShingle Articles
Savarensky, E. F.
Proskuryakova, T. A.
Glasko, V. B.
Granit, Y. Sh.
Voronina, E. V.
On the Lateral Refraction of Rayleigh Surface Waves and Microseisms in the North Atlantic
topic_facet Articles
description The lateral refraction of microseisms with T = 6 s and of surface waves with T = 20 s has been computed for North Atlantic sources recorded at European stations (Pulkovo, Simferopol, Prague). Such surface waves are not always recorded at certain stations for all source regions owing to the peculiarities of wave propagation. These pecularities should be taken into account when tracing the sources of North Atlantic microseisms.
format Text
author Savarensky, E. F.
Proskuryakova, T. A.
Glasko, V. B.
Granit, Y. Sh.
Voronina, E. V.
author_facet Savarensky, E. F.
Proskuryakova, T. A.
Glasko, V. B.
Granit, Y. Sh.
Voronina, E. V.
author_sort Savarensky, E. F.
title On the Lateral Refraction of Rayleigh Surface Waves and Microseisms in the North Atlantic
title_short On the Lateral Refraction of Rayleigh Surface Waves and Microseisms in the North Atlantic
title_full On the Lateral Refraction of Rayleigh Surface Waves and Microseisms in the North Atlantic
title_fullStr On the Lateral Refraction of Rayleigh Surface Waves and Microseisms in the North Atlantic
title_full_unstemmed On the Lateral Refraction of Rayleigh Surface Waves and Microseisms in the North Atlantic
title_sort on the lateral refraction of rayleigh surface waves and microseisms in the north atlantic
publisher Oxford University Press
publishDate 1968
url http://gji.oxfordjournals.org/cgi/content/short/15/5/529
https://doi.org/10.1111/j.1365-246X.1968.tb00207.x
genre North Atlantic
genre_facet North Atlantic
op_relation http://gji.oxfordjournals.org/cgi/content/short/15/5/529
http://dx.doi.org/10.1111/j.1365-246X.1968.tb00207.x
op_rights Copyright (C) 1968, Oxford University Press
op_doi https://doi.org/10.1111/j.1365-246X.1968.tb00207.x
container_title Geophysical Journal International
container_volume 15
container_issue 5
container_start_page 529
op_container_end_page 544
_version_ 1766117139289210880

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