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1. Identity statement
Reference TypeBook Section
Siteplutao.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentifierJ8LNKB5R7W/3Q6397B
Repositoryurlib.net/www/2017/12.05.13.58.57   (restricted access)
Last Update2018:08.30.13.16.14 (UTC) simone
Metadata Repositoryurlib.net/www/2017/12.05.13.58.58
Metadata Last Update2018:08.30.13.16.15 (UTC) simone
ISBN9783319578217
Labellattes: 5348874855184718 1 KlausnerSaMeKhPiMu:2017:InMaFi
Citation KeyKlausnerSaMeKhPiMu:2017:InMaFi
TitleChile2015: induced magnetic fields on Z component by tsunami wave propagation
Year2017
Access Date2024, May 08
Secondary TypePRE LI
Number of Files1
Size6017 KiB
2. Context
Author1 Klausner, Virginia
2 Santos, Thiago Almeida dos
3 Meneses Júnior, Francisco Carlos de
4 Kherani, Esfhan Alan
5 Pillat, Valdir Gil
6 Muella, M. T. A. H.
Group1
2
3 DIDAE-CGCEA-INPE-MCTIC-GOV-BR
4 DIDAE-CGCEA-INPE-MCTIC-GOV-BR
Affiliation1 Universidade do Vale do Paraíba (UNIVAP)
2 Universidade do Vale do Paraíba (UNIVAP)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 Universidade do Vale do Paraíba (UNIVAP)
6 Universidade do Vale do Paraíba (UNIVAP)
Author e-Mail Address1
2
3 francisco.meneses@inpe.br
4 esfhan.kherani@inpe.br
EditorBraitenberg, Carla
Rabinovich, Alexander B.
Book TitleThe Chile-2015 (Illapel) Earthquake and Tsunami
PublisherSpringer International Publishing
CityCham, Suiça
Pages193-208
History (UTC)2017-12-14 15:48:11 :: lattes -> administrator :: 2017
2018-06-04 23:26:41 :: administrator -> simone :: 2017
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsChilean tsunami 2015
tsunamigenic magnetic disturbances
Z-component
tavelet analysis
effectiveness wavelet coefficients
AbstractThis study reports the magnetic disturbances due to the Chilean tsunami (2015). Using 10 ground-based magnetometer observatories spread in the Pacific Ocean, covering approximately 150º epicentral distance, for a time duration of 24 h from the tsunami initiation, tsunamigenic disturbances in the Z-component of the geomagnetic field are investigated. The methodologies namely, the discrete wavelet transform (DWT), the newly developed approach called effectiveness wavelet coefficient (EWC), and intrinsic mode functions (IMF) decomposition are implemented to detect these tsunamigenic disturbances. The analysis reveals the presence of an increase of EWC amplitude due to tsunamigenic magnetic disturbances nearly around the tsunami arrival time at each observatory. The IMF decomposition analysis using 1040 min levels of decomposition shows the amplified magnetic disturbances around the time of the increase in EWC amplitude. In most of the observatories, the time of the amplified EWC is consistent with the approximate time of the tsunami arrival, while in the other observatories, the IMF decomposition provides better consistency. The results suggest that the methodologies implemented in the present work can be effectively used to characterize the tsunamigenic contributions in the geomagnetic field, since the tsunami wavefront propagates towards the Pacific Ocean covers the time duration as long as 24 h from the tsunami initiation.
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDAE > Chile2015: induced magnetic...
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4. Conditions of access and use
Languagept
User Grouplattes
Visibilityshown
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ETL868
URL (untrusted data)https://books.google.com.mx/books?id=vSnBAQAACAAJ
Host Collectiondpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notes
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