Rapid estimation of source parameters for the 2022 Mw 6.6 Menyuan earthquake with combined high-rate GNSS and strong motion data in Northeastern Tibet.

Saved in:
Bibliographic Details
Title: Rapid estimation of source parameters for the 2022 Mw 6.6 Menyuan earthquake with combined high-rate GNSS and strong motion data in Northeastern Tibet.
Authors: Yang, Chen1 (AUTHOR), Su, Xiaoning1,2 (AUTHOR) suxiaoning_666@126.com, Gao, Zhiyu1,2 (AUTHOR), Kou, Ruixiong1,2 (AUTHOR)
Source: Terrestrial, Atmospheric & Oceanic Sciences. 12/20/2024, Vol. 35 Issue 1, p1-12. 12p.
Subjects: Global Positioning System, Magnitude estimation, Earthquakes, Parameter estimation, Emergency management
Abstract: To investigate the reliability of high-rate GNSS in the rapid estimation of source parameters for the 2022 Menyuan Mw 6.6 earthquake, we collected high-rate GNSS and strong motion data within a 200 km radius of the epicenter. We performed high-precision calculations to obtain three-dimensional dynamic displacement waveforms for all stations and analyzed the reliability of source parameter estimation and coseismic deformation acquisition. The three-dimensional dynamic displacement waveforms show that the amplitude of displacement fluctuations at each station decreases with increasing distance from the epicenter. The station closest to the epicenter, C007, recorded a maximum east–west amplitude of 15 cm, a north–south amplitude of 10.8 cm, and a vertical amplitude of only 2.2 cm. The inverted epicenter location using displacement waveforms is (101.263°E, 37.802°N), with an origin time of 17:45:25.9 (UTC) and a magnitude of Mw 6.65. These results are generally consistent with those obtained from seismological methods using the seismic data. By combining high-rate GNSS and strong-motion data for magnitude estimation, an initial value of Mw 6.0 can be obtained 15 s after the earthquake, with stable convergence to Mw 6.6 within 40 s. The quality of magnitude estimation convergence is positively correlated with the number of stations. Based on the displacement waveforms 100 s before and after the earthquake, the coseismic deformation of this event can be quickly obtained. The results show opposite motion trends on the south and north sides of the seismogenic fault, with no significant vertical movement. Our results indicate that using near-field high-rate GNSS and strong motion data can rapidly and effectively estimate the source parameters and coseismic deformation of the strong earthquake, which can provide valuable reference for post-earthquake emergency response and rapid disaster assessment. [ABSTRACT FROM AUTHOR]
Copyright of Terrestrial, Atmospheric & Oceanic Sciences is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
Database: Engineering Source
Full text is not displayed to guests.
FullText Links:
  – Type: pdflink
Text:
  Availability: 1
Header DbId: egs
DbLabel: Engineering Source
An: 181826291
AccessLevel: 6
PubType: Academic Journal
PubTypeId: academicJournal
PreciseRelevancyScore: 0
IllustrationInfo
Items – Name: Title
  Label: Title
  Group: Ti
  Data: Rapid estimation of source parameters for the 2022 Mw 6.6 Menyuan earthquake with combined high-rate GNSS and strong motion data in Northeastern Tibet.
– Name: Author
  Label: Authors
  Group: Au
  Data: <searchLink fieldCode="AR" term="%22Yang%2C+Chen%22">Yang, Chen</searchLink><relatesTo>1</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Su%2C+Xiaoning%22">Su, Xiaoning</searchLink><relatesTo>1,2</relatesTo> (AUTHOR)<i> suxiaoning_666@126.com</i><br /><searchLink fieldCode="AR" term="%22Gao%2C+Zhiyu%22">Gao, Zhiyu</searchLink><relatesTo>1,2</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Kou%2C+Ruixiong%22">Kou, Ruixiong</searchLink><relatesTo>1,2</relatesTo> (AUTHOR)
– Name: TitleSource
  Label: Source
  Group: Src
  Data: <searchLink fieldCode="JN" term="%22Terrestrial%2C+Atmospheric+%26+Oceanic+Sciences%22">Terrestrial, Atmospheric & Oceanic Sciences</searchLink>. 12/20/2024, Vol. 35 Issue 1, p1-12. 12p.
– Name: Subject
  Label: Subjects
  Group: Su
  Data: <searchLink fieldCode="DE" term="%22Global+Positioning+System%22">Global Positioning System</searchLink><br /><searchLink fieldCode="DE" term="%22Magnitude+estimation%22">Magnitude estimation</searchLink><br /><searchLink fieldCode="DE" term="%22Earthquakes%22">Earthquakes</searchLink><br /><searchLink fieldCode="DE" term="%22Parameter+estimation%22">Parameter estimation</searchLink><br /><searchLink fieldCode="DE" term="%22Emergency+management%22">Emergency management</searchLink>
– Name: Abstract
  Label: Abstract
  Group: Ab
  Data: To investigate the reliability of high-rate GNSS in the rapid estimation of source parameters for the 2022 Menyuan Mw 6.6 earthquake, we collected high-rate GNSS and strong motion data within a 200 km radius of the epicenter. We performed high-precision calculations to obtain three-dimensional dynamic displacement waveforms for all stations and analyzed the reliability of source parameter estimation and coseismic deformation acquisition. The three-dimensional dynamic displacement waveforms show that the amplitude of displacement fluctuations at each station decreases with increasing distance from the epicenter. The station closest to the epicenter, C007, recorded a maximum east–west amplitude of 15 cm, a north–south amplitude of 10.8 cm, and a vertical amplitude of only 2.2 cm. The inverted epicenter location using displacement waveforms is (101.263°E, 37.802°N), with an origin time of 17:45:25.9 (UTC) and a magnitude of Mw 6.65. These results are generally consistent with those obtained from seismological methods using the seismic data. By combining high-rate GNSS and strong-motion data for magnitude estimation, an initial value of Mw 6.0 can be obtained 15 s after the earthquake, with stable convergence to Mw 6.6 within 40 s. The quality of magnitude estimation convergence is positively correlated with the number of stations. Based on the displacement waveforms 100 s before and after the earthquake, the coseismic deformation of this event can be quickly obtained. The results show opposite motion trends on the south and north sides of the seismogenic fault, with no significant vertical movement. Our results indicate that using near-field high-rate GNSS and strong motion data can rapidly and effectively estimate the source parameters and coseismic deformation of the strong earthquake, which can provide valuable reference for post-earthquake emergency response and rapid disaster assessment. [ABSTRACT FROM AUTHOR]
– Name: AbstractSuppliedCopyright
  Label:
  Group: Ab
  Data: <i>Copyright of Terrestrial, Atmospheric & Oceanic Sciences is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
PLink https://search.ebscohost.com/login.aspx?direct=true&site=eds-live&db=egs&AN=181826291
RecordInfo BibRecord:
  BibEntity:
    Identifiers:
      – Type: doi
        Value: 10.1007/s44195-024-00083-5
    Languages:
      – Code: eng
        Text: English
    PhysicalDescription:
      Pagination:
        PageCount: 12
        StartPage: 1
    Subjects:
      – SubjectFull: Global Positioning System
        Type: general
      – SubjectFull: Magnitude estimation
        Type: general
      – SubjectFull: Earthquakes
        Type: general
      – SubjectFull: Parameter estimation
        Type: general
      – SubjectFull: Emergency management
        Type: general
    Titles:
      – TitleFull: Rapid estimation of source parameters for the 2022 Mw 6.6 Menyuan earthquake with combined high-rate GNSS and strong motion data in Northeastern Tibet.
        Type: main
  BibRelationships:
    HasContributorRelationships:
      – PersonEntity:
          Name:
            NameFull: Yang, Chen
      – PersonEntity:
          Name:
            NameFull: Su, Xiaoning
      – PersonEntity:
          Name:
            NameFull: Gao, Zhiyu
      – PersonEntity:
          Name:
            NameFull: Kou, Ruixiong
    IsPartOfRelationships:
      – BibEntity:
          Dates:
            – D: 20
              M: 12
              Text: 12/20/2024
              Type: published
              Y: 2024
          Identifiers:
            – Type: issn-print
              Value: 10170839
          Numbering:
            – Type: volume
              Value: 35
            – Type: issue
              Value: 1
          Titles:
            – TitleFull: Terrestrial, Atmospheric & Oceanic Sciences
              Type: main
ResultId 1