Long Period Microseisms in Southern Norway

Sea wave recordings from the Norwegian Coast and seismic recordings from the long period instruments of the Norwegian Seismic Array (NORSAR) and from the new broad band long period instruments at Kongsberg have been used to study the characteristics and the source locations of long period microseism...

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Bibliographic Details
Main Authors: Rygg, Elvind, Bruland, Leif
Other Authors: BERGEN UNIV (NORWAY) SEISMOLOGICAL OBSERVATORY
Format: Text
Language:English
Published: 1974
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA000026
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA000026
id ftdtic:ADA000026
record_format openpolar
spelling ftdtic:ADA000026 2023-05-15T16:49:15+02:00 Long Period Microseisms in Southern Norway Rygg, Elvind Bruland, Leif BERGEN UNIV (NORWAY) SEISMOLOGICAL OBSERVATORY 1974-05-31 text/html http://www.dtic.mil/docs/citations/ADA000026 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA000026 en eng http://www.dtic.mil/docs/citations/ADA000026 Approved for public release; distribution is unlimited. DTIC AND NTIS Seismology *MICROSEISMS *NORWAY ANOMALIES BROADBAND COASTAL REGIONS CORRELATION TECHNIQUES FREQUENCY OCEAN WAVES SEISMIC ARRAYS SEISMIC DATA SEISMIC DETECTION SEISMOLOGICAL STATIONS SEISMOMETERS SOURCES Norwegian seismic array Kongsberg(Norway) Long period seismometers Text 1974 ftdtic 2016-02-24T14:10:44Z Sea wave recordings from the Norwegian Coast and seismic recordings from the long period instruments of the Norwegian Seismic Array (NORSAR) and from the new broad band long period instruments at Kongsberg have been used to study the characteristics and the source locations of long period microseisms in Southern Norway. The disturbances associated with lows in the Lofoten - Vesteralen area normally generate large, regular wave packets (beats) of double frequency (DF), 0.12-0.16 Hz, microseisms at Kongsberg. Meteorological disturbances in the British Isles - Iceland area often generate large PF microseisms and moderate, irregular DF microseisms. Occasionally the sea waves at the West Coast of Norway are sufficiently long period to generage PF microseisms. Text Iceland Lofoten Defense Technical Information Center: DTIC Technical Reports database Kongsberg ENVELOPE(19.082,19.082,69.123,69.123) Lofoten Norway
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Seismology
*MICROSEISMS
*NORWAY
ANOMALIES
BROADBAND
COASTAL REGIONS
CORRELATION TECHNIQUES
FREQUENCY
OCEAN WAVES
SEISMIC ARRAYS
SEISMIC DATA
SEISMIC DETECTION
SEISMOLOGICAL STATIONS
SEISMOMETERS
SOURCES
Norwegian seismic array
Kongsberg(Norway)
Long period seismometers
spellingShingle Seismology
*MICROSEISMS
*NORWAY
ANOMALIES
BROADBAND
COASTAL REGIONS
CORRELATION TECHNIQUES
FREQUENCY
OCEAN WAVES
SEISMIC ARRAYS
SEISMIC DATA
SEISMIC DETECTION
SEISMOLOGICAL STATIONS
SEISMOMETERS
SOURCES
Norwegian seismic array
Kongsberg(Norway)
Long period seismometers
Rygg, Elvind
Bruland, Leif
Long Period Microseisms in Southern Norway
topic_facet Seismology
*MICROSEISMS
*NORWAY
ANOMALIES
BROADBAND
COASTAL REGIONS
CORRELATION TECHNIQUES
FREQUENCY
OCEAN WAVES
SEISMIC ARRAYS
SEISMIC DATA
SEISMIC DETECTION
SEISMOLOGICAL STATIONS
SEISMOMETERS
SOURCES
Norwegian seismic array
Kongsberg(Norway)
Long period seismometers
description Sea wave recordings from the Norwegian Coast and seismic recordings from the long period instruments of the Norwegian Seismic Array (NORSAR) and from the new broad band long period instruments at Kongsberg have been used to study the characteristics and the source locations of long period microseisms in Southern Norway. The disturbances associated with lows in the Lofoten - Vesteralen area normally generate large, regular wave packets (beats) of double frequency (DF), 0.12-0.16 Hz, microseisms at Kongsberg. Meteorological disturbances in the British Isles - Iceland area often generate large PF microseisms and moderate, irregular DF microseisms. Occasionally the sea waves at the West Coast of Norway are sufficiently long period to generage PF microseisms.
author2 BERGEN UNIV (NORWAY) SEISMOLOGICAL OBSERVATORY
format Text
author Rygg, Elvind
Bruland, Leif
author_facet Rygg, Elvind
Bruland, Leif
author_sort Rygg, Elvind
title Long Period Microseisms in Southern Norway
title_short Long Period Microseisms in Southern Norway
title_full Long Period Microseisms in Southern Norway
title_fullStr Long Period Microseisms in Southern Norway
title_full_unstemmed Long Period Microseisms in Southern Norway
title_sort long period microseisms in southern norway
publishDate 1974
url http://www.dtic.mil/docs/citations/ADA000026
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA000026
long_lat ENVELOPE(19.082,19.082,69.123,69.123)
geographic Kongsberg
Lofoten
Norway
geographic_facet Kongsberg
Lofoten
Norway
genre Iceland
Lofoten
genre_facet Iceland
Lofoten
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA000026
op_rights Approved for public release; distribution is unlimited.
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