FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2044678763> ?p ?o ?g. }

• W2044678763 abstract "We study the origin of the background seismic noise averaged over long time by cross correlating of the vertical component of motion, which were first normalized by 1‐bit coding. We use 1 year of recording at several stations of networks located in North America, western Europe, and Tanzania. We measure normalized amplitudes of Rayleigh waves reconstructed from correlation for all available station to station paths within the networks for positive and negative correlation times to determine the seasonally averaged azimuthal distribution of normalized background energy flow (NBEF) through the networks. We perform the analysis for the two spectral bands corresponding to the primary (10–20 s) and secondary (5–10 s) microseism and also for the 20–40 s band. The direction of the NBEF for the strongest spectral peak between 5 and 10 s is found to be very stable in time with signal mostly coming from the coastline, confirming that the secondary microseism is generated by the nonlinear interaction of the ocean swell with the coast. At the same time, the NBEF in the band of the primary microseism (10–20 s) has a very clear seasonal variability very similar to the behavior of the long‐period (20–40 s) noise. This suggests that contrary to the secondary microseism, the primary microseism is not produced by a direct effect of the swell incident on coastlines but rather by the same process that generates the longer‐period noise. By simultaneously analyzing networks in California, eastern United States, Europe, and Tanzania we are able to identify main source regions of the 10–20 s noise. They are located in the northern Atlantic and in the northern Pacific during the winter and in the Indian Ocean and in southern Pacific during the summer. These distributions of sources share a great similarity with the map of average ocean wave height map obtained by TOPEX‐Poseidon. This suggests that the seismic noise for periods larger than 10 s is clearly related to ocean wave activity in deep water. The mechanism of its generation is likely to be similar to the one proposed for larger periods, namely, infragravity ocean waves." @default.
• W2044678763 created "2016-06-24" @default.
• W2044678763 creator A5031082257 @default.
• W2044678763 creator A5044344584 @default.
• W2044678763 creator A5046672035 @default.
• W2044678763 date "2006-10-01" @default.
• W2044678763 modified "2023-10-16" @default.
• W2044678763 title "A study of the seismic noise from its long-range correlation properties" @default.
• W2044678763 cites W1499749804 @default.
• W2044678763 cites W1514036343 @default.
• W2044678763 cites W1536121380 @default.
• W2044678763 cites W1544293143 @default.
• W2044678763 cites W1695352019 @default.
• W2044678763 cites W1730109095 @default.
• W2044678763 cites W1836947475 @default.
• W2044678763 cites W1844897206 @default.
• W2044678763 cites W1975482522 @default.
• W2044678763 cites W1983958061 @default.
• W2044678763 cites W1987494683 @default.
• W2044678763 cites W1990446599 @default.
• W2044678763 cites W2005926772 @default.
• W2044678763 cites W2010733296 @default.
• W2044678763 cites W2036360358 @default.
• W2044678763 cites W2047645263 @default.
• W2044678763 cites W2053548331 @default.
• W2044678763 cites W2057516589 @default.
• W2044678763 cites W2061944577 @default.
• W2044678763 cites W2065126285 @default.
• W2044678763 cites W2074504886 @default.
• W2044678763 cites W2074604051 @default.
• W2044678763 cites W2086404904 @default.
• W2044678763 cites W2093575409 @default.
• W2044678763 cites W2099307303 @default.
• W2044678763 cites W2119560458 @default.
• W2044678763 cites W2139260764 @default.
• W2044678763 cites W2158649092 @default.
• W2044678763 cites W2160567428 @default.
• W2044678763 cites W2487375839 @default.
• W2044678763 cites W57061860 @default.
• W2044678763 doi "https://doi.org/10.1029/2005jb004237" @default.
• W2044678763 hasPublicationYear "2006" @default.
• W2044678763 type Work @default.
• W2044678763 sameAs 2044678763 @default.
• W2044678763 citedByCount "438" @default.
• W2044678763 countsByYear W20446787632012 @default.
• W2044678763 countsByYear W20446787632013 @default.
• W2044678763 countsByYear W20446787632014 @default.
• W2044678763 countsByYear W20446787632015 @default.
• W2044678763 countsByYear W20446787632016 @default.
• W2044678763 countsByYear W20446787632017 @default.
• W2044678763 countsByYear W20446787632018 @default.
• W2044678763 countsByYear W20446787632019 @default.
• W2044678763 countsByYear W20446787632020 @default.
• W2044678763 countsByYear W20446787632021 @default.
• W2044678763 countsByYear W20446787632022 @default.
• W2044678763 countsByYear W20446787632023 @default.
• W2044678763 crossrefType "journal-article" @default.
• W2044678763 hasAuthorship W2044678763A5031082257 @default.
• W2044678763 hasAuthorship W2044678763A5044344584 @default.
• W2044678763 hasAuthorship W2044678763A5046672035 @default.
• W2044678763 hasBestOaLocation W20446787631 @default.
• W2044678763 hasConcept C108628306 @default.
• W2044678763 hasConcept C111368507 @default.
• W2044678763 hasConcept C115961682 @default.
• W2044678763 hasConcept C120665830 @default.
• W2044678763 hasConcept C121332964 @default.
• W2044678763 hasConcept C127313418 @default.
• W2044678763 hasConcept C13280743 @default.
• W2044678763 hasConcept C154945302 @default.
• W2044678763 hasConcept C159737794 @default.
• W2044678763 hasConcept C165205528 @default.
• W2044678763 hasConcept C180205008 @default.
• W2044678763 hasConcept C184652730 @default.
• W2044678763 hasConcept C203718221 @default.
• W2044678763 hasConcept C205312793 @default.
• W2044678763 hasConcept C2524010 @default.
• W2044678763 hasConcept C30947920 @default.
• W2044678763 hasConcept C33923547 @default.
• W2044678763 hasConcept C41008148 @default.
• W2044678763 hasConcept C44886760 @default.
• W2044678763 hasConcept C51473458 @default.
• W2044678763 hasConcept C62520636 @default.
• W2044678763 hasConcept C7266685 @default.
• W2044678763 hasConcept C83176761 @default.
• W2044678763 hasConcept C99498987 @default.
• W2044678763 hasConceptScore W2044678763C108628306 @default.
• W2044678763 hasConceptScore W2044678763C111368507 @default.
• W2044678763 hasConceptScore W2044678763C115961682 @default.
• W2044678763 hasConceptScore W2044678763C120665830 @default.
• W2044678763 hasConceptScore W2044678763C121332964 @default.
• W2044678763 hasConceptScore W2044678763C127313418 @default.
• W2044678763 hasConceptScore W2044678763C13280743 @default.
• W2044678763 hasConceptScore W2044678763C154945302 @default.
• W2044678763 hasConceptScore W2044678763C159737794 @default.
• W2044678763 hasConceptScore W2044678763C165205528 @default.
• W2044678763 hasConceptScore W2044678763C180205008 @default.
• W2044678763 hasConceptScore W2044678763C184652730 @default.
• W2044678763 hasConceptScore W2044678763C203718221 @default.
• W2044678763 hasConceptScore W2044678763C205312793 @default.
• W2044678763 hasConceptScore W2044678763C2524010 @default.

• next