FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2314213040> ?p ?o ?g. }

• W2314213040 endingPage "1491" @default.
• W2314213040 startingPage "1473" @default.
• W2314213040 abstract "We introduce a method for mapping the noise-source distribution of microseisms which uses information from the full length of covariograms (cross-correlations). We derive a forward calculation based on the plane-wave assumption in 2-D, to formulate an iterative, linearized inversion of covariogram envelopes in the time domain. The forward calculation involves bandpass filtering of the covariograms. The inversion exploits the well-known feature of noise cross-correlation, that is, an anomaly in the noise field that is oblique to the interstation direction appears as cross-correlation amplitude at a smaller time lag than the in-line, surface wave arrival. Therefore, the inversion extracts more information from the covariograms than that contained at the expected surface wave arrival, and this allows us to work with few stations to find the propagation directions of incoming energy. The inversion is naturally applied to data that retain physical units that are not amplitude normalized in any way. By dividing a network into groups of stations, we can constrain the source location by triangulation. We demonstrate results of the method with synthetic data and one year (2012) of data from the Swedish National Seismic Network and also look at the seasonal variation of source distribution around Scandinavia. After preprocessing and cross-correlation, the stations are divided into five groups of 9–12 stations. We invert the envelopes of each group in eight period ranges between 2 and 25 s. Results show that the noise sources at short periods (less than 12 s) lie predominantly in the North Atlantic Ocean and the Barents Sea, and at longer periods the energy appears to have a broader distribution. The strongly anisotropic source distribution in this area is estimated to cause significant biases of velocity measurements compared to the level of heterogeneity in the region. The amplitude of the primary microseisms varies little over the year, but secondary microseisms are much weaker in summer than in winter. Furthermore, the peak period of the secondary microseisms shifts from 5–6 s in winter to 4–5 s during the summer." @default.
• W2314213040 created "2016-06-24" @default.
• W2314213040 creator A5002840041 @default.
• W2314213040 creator A5011073337 @default.
• W2314213040 creator A5059638591 @default.
• W2314213040 creator A5073043860 @default.
• W2314213040 date "2016-03-07" @default.
• W2314213040 modified "2023-10-16" @default.
• W2314213040 title "Mapping the source distribution of microseisms using noise covariogram envelopes" @default.
• W2314213040 cites W1514036343 @default.
• W2314213040 cites W1522271460 @default.
• W2314213040 cites W1558521841 @default.
• W2314213040 cites W1583639331 @default.
• W2314213040 cites W1595921706 @default.
• W2314213040 cites W1606469409 @default.
• W2314213040 cites W1824223748 @default.
• W2314213040 cites W1838138324 @default.
• W2314213040 cites W1924737941 @default.
• W2314213040 cites W1948753488 @default.
• W2314213040 cites W1960107577 @default.
• W2314213040 cites W1964195730 @default.
• W2314213040 cites W1968843244 @default.
• W2314213040 cites W1970727905 @default.
• W2314213040 cites W1973202980 @default.
• W2314213040 cites W1974568218 @default.
• W2314213040 cites W1979440239 @default.
• W2314213040 cites W1999009360 @default.
• W2314213040 cites W2005926772 @default.
• W2314213040 cites W2008095626 @default.
• W2314213040 cites W2016727966 @default.
• W2314213040 cites W2018012328 @default.
• W2314213040 cites W2022835545 @default.
• W2314213040 cites W2023388655 @default.
• W2314213040 cites W2024219064 @default.
• W2314213040 cites W2029660105 @default.
• W2314213040 cites W2037094469 @default.
• W2314213040 cites W2037630069 @default.
• W2314213040 cites W2044678763 @default.
• W2314213040 cites W2045618492 @default.
• W2314213040 cites W2046728195 @default.
• W2314213040 cites W2048200609 @default.
• W2314213040 cites W2061777253 @default.
• W2314213040 cites W2065126285 @default.
• W2314213040 cites W2082374900 @default.
• W2314213040 cites W2083769537 @default.
• W2314213040 cites W2084215135 @default.
• W2314213040 cites W2095628723 @default.
• W2314213040 cites W2100374497 @default.
• W2314213040 cites W2102472030 @default.
• W2314213040 cites W2110669974 @default.
• W2314213040 cites W2113987786 @default.
• W2314213040 cites W2117573189 @default.
• W2314213040 cites W2120062664 @default.
• W2314213040 cites W2122622153 @default.
• W2314213040 cites W2125124331 @default.
• W2314213040 cites W2125569072 @default.
• W2314213040 cites W2126487354 @default.
• W2314213040 cites W2126562184 @default.
• W2314213040 cites W2128913609 @default.
• W2314213040 cites W2129155621 @default.
• W2314213040 cites W2131006763 @default.
• W2314213040 cites W2134437781 @default.
• W2314213040 cites W2139713088 @default.
• W2314213040 cites W2140552722 @default.
• W2314213040 cites W2141247629 @default.
• W2314213040 cites W2141845572 @default.
• W2314213040 cites W2150047080 @default.
• W2314213040 cites W2153328878 @default.
• W2314213040 cites W2153806527 @default.
• W2314213040 cites W2157115677 @default.
• W2314213040 cites W2160567428 @default.
• W2314213040 cites W2168379187 @default.
• W2314213040 cites W2334672533 @default.
• W2314213040 cites W3021374494 @default.
• W2314213040 doi "https://doi.org/10.1093/gji/ggw092" @default.
• W2314213040 hasPublicationYear "2016" @default.
• W2314213040 type Work @default.
• W2314213040 sameAs 2314213040 @default.
• W2314213040 citedByCount "14" @default.
• W2314213040 countsByYear W23142130402017 @default.
• W2314213040 countsByYear W23142130402018 @default.
• W2314213040 countsByYear W23142130402020 @default.
• W2314213040 countsByYear W23142130402021 @default.
• W2314213040 countsByYear W23142130402022 @default.
• W2314213040 countsByYear W23142130402023 @default.
• W2314213040 crossrefType "journal-article" @default.
• W2314213040 hasAuthorship W2314213040A5002840041 @default.
• W2314213040 hasAuthorship W2314213040A5011073337 @default.
• W2314213040 hasAuthorship W2314213040A5059638591 @default.
• W2314213040 hasAuthorship W2314213040A5073043860 @default.
• W2314213040 hasBestOaLocation W23142130401 @default.
• W2314213040 hasConcept C115961682 @default.
• W2314213040 hasConcept C120665830 @default.
• W2314213040 hasConcept C121332964 @default.
• W2314213040 hasConcept C127313418 @default.
• W2314213040 hasConcept C13280743 @default.
• W2314213040 hasConcept C134306372 @default.
• W2314213040 hasConcept C154945302 @default.

• next