T-WAVE GENERATION MECHANISMS
The transformation of earthquake body waves to T waves is as efficient at deep slopes as at slopes which transect the sofar axis. Moreover, spectral studies of T phase signatures have shown no basis for distinguishing between the two cases. As simple downslope propagation is inadequate to explain th...
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ftdtic:AD0708695 2023-05-15T18:28:10+02:00 T-WAVE GENERATION MECHANISMS Johnson, Rockne H. Norris, Roger A. HAWAII INST OF GEOPHYSICS HONOLULU 1970-01 text/html http://www.dtic.mil/docs/citations/AD0708695 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0708695 en eng http://www.dtic.mil/docs/citations/AD0708695 Approved for public release; distribution is unlimited. DTIC AND NTIS Seismology *SEISMIC WAVES *PACIFIC OCEAN PROPAGATION MEASUREMENT HIGH FREQUENCY HYDROPHONES SPECTRUM SIGNATURES OCEAN BOTTOM TOPOGRAPHY EPICENTERS INTENSITY REFLECTION SURFACE PROPERTIES *EAST PACIFIC RISE SONAGRAMS SPECTRUM ANALYSIS T WAVES Text 1970 ftdtic 2016-02-22T01:35:58Z The transformation of earthquake body waves to T waves is as efficient at deep slopes as at slopes which transect the sofar axis. Moreover, spectral studies of T phase signatures have shown no basis for distinguishing between the two cases. As simple downslope propagation is inadequate to explain the production of T waves at deep slopes, that process is relegated a minor role in favor of scattering from the sea floor as the dominant mechanism. A slope in the direction of propagation insures that once energy is scattered in that direction the probability of its being unfavorably rescattered upon successive approaches to the sea floor will be less. Scattering near the sea surface is detectable in the absence of bottom-scattered T waves. Such abyssally generated T waves display a distinctly higher frequency spectrum when originating in subarctic regions than when originating in lower latitudes. This difference is ascribed to downward ducting of higher frequency energy from the subarctic surface channel. Text Subarctic Defense Technical Information Center: DTIC Technical Reports database Pacific |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Seismology *SEISMIC WAVES *PACIFIC OCEAN PROPAGATION MEASUREMENT HIGH FREQUENCY HYDROPHONES SPECTRUM SIGNATURES OCEAN BOTTOM TOPOGRAPHY EPICENTERS INTENSITY REFLECTION SURFACE PROPERTIES *EAST PACIFIC RISE SONAGRAMS SPECTRUM ANALYSIS T WAVES |
spellingShingle |
Seismology *SEISMIC WAVES *PACIFIC OCEAN PROPAGATION MEASUREMENT HIGH FREQUENCY HYDROPHONES SPECTRUM SIGNATURES OCEAN BOTTOM TOPOGRAPHY EPICENTERS INTENSITY REFLECTION SURFACE PROPERTIES *EAST PACIFIC RISE SONAGRAMS SPECTRUM ANALYSIS T WAVES Johnson, Rockne H. Norris, Roger A. T-WAVE GENERATION MECHANISMS |
topic_facet |
Seismology *SEISMIC WAVES *PACIFIC OCEAN PROPAGATION MEASUREMENT HIGH FREQUENCY HYDROPHONES SPECTRUM SIGNATURES OCEAN BOTTOM TOPOGRAPHY EPICENTERS INTENSITY REFLECTION SURFACE PROPERTIES *EAST PACIFIC RISE SONAGRAMS SPECTRUM ANALYSIS T WAVES |
description |
The transformation of earthquake body waves to T waves is as efficient at deep slopes as at slopes which transect the sofar axis. Moreover, spectral studies of T phase signatures have shown no basis for distinguishing between the two cases. As simple downslope propagation is inadequate to explain the production of T waves at deep slopes, that process is relegated a minor role in favor of scattering from the sea floor as the dominant mechanism. A slope in the direction of propagation insures that once energy is scattered in that direction the probability of its being unfavorably rescattered upon successive approaches to the sea floor will be less. Scattering near the sea surface is detectable in the absence of bottom-scattered T waves. Such abyssally generated T waves display a distinctly higher frequency spectrum when originating in subarctic regions than when originating in lower latitudes. This difference is ascribed to downward ducting of higher frequency energy from the subarctic surface channel. |
author2 |
HAWAII INST OF GEOPHYSICS HONOLULU |
format |
Text |
author |
Johnson, Rockne H. Norris, Roger A. |
author_facet |
Johnson, Rockne H. Norris, Roger A. |
author_sort |
Johnson, Rockne H. |
title |
T-WAVE GENERATION MECHANISMS |
title_short |
T-WAVE GENERATION MECHANISMS |
title_full |
T-WAVE GENERATION MECHANISMS |
title_fullStr |
T-WAVE GENERATION MECHANISMS |
title_full_unstemmed |
T-WAVE GENERATION MECHANISMS |
title_sort |
t-wave generation mechanisms |
publishDate |
1970 |
url |
http://www.dtic.mil/docs/citations/AD0708695 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0708695 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Subarctic |
genre_facet |
Subarctic |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0708695 |
op_rights |
Approved for public release; distribution is unlimited. |
_version_ |
1766210547930365952 |