Item talk:Q45641: Difference between revisions

From geokb
(Updated person data cache with ORCID information)
(Updated item talk page content)
Line 3,766: Line 3,766:
usgs_staff_profile:
usgs_staff_profile:
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   meta:
    url: https://www.usgs.gov/staff-profiles/phillip-dawson
    timestamp: '2024-01-30T13:13:21.706412'
     status_code: 200
     status_code: 200
    timestamp: '2023-09-30T17:05:18.028794'
    url: https://www.usgs.gov/staff-profiles/phillip-dawson
   profile:
   profile:
     abstracts: []
     name: Phillip Dawson, IV
     affiliations: []
     name_qualifier: null
     education: []
     titles:
    - Volcano Seismologist
    organizations:
    - !!python/tuple
      - California Volcano Observatory
      - https://www.usgs.gov/observatories/calvo
     email: dawson@usgs.gov
     email: dawson@usgs.gov
    orcid: 0000-0003-4065-0588
    intro_statements:
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      \ active volcanism and volcanic processes."
     expertise_terms:
     expertise_terms:
     - Volcano Seismology
     - Volcano Seismology
     - Seismic tomography
     - Seismic tomography
    professional_experience: []
    education: []
    affiliations: []
     honors: []
     honors: []
     intro_statements:
     abstracts: []
    - "Phillip Dawson is a geophysicist with the U.S. Geological Survey\u2019s Volcano\
      \ Science Center, focusing on theoretical and experimental investigations of\
      \ active volcanism and volcanic processes."
    name: Phillip Dawson, IV
    name_qualifier: null
    orcid: 0000-0003-4065-0588
    organization_link: https://www.usgs.gov/observatories/calvo
    organization_name: California Volcano Observatory
     personal_statement: 'Phillip Dawson hails from a small town located on the flank
     personal_statement: 'Phillip Dawson hails from a small town located on the flank
       of one of the world''s largest stratovolcanoes - Mount Shasta, California.  Who
       of one of the world''s largest stratovolcanoes - Mount Shasta, California.  Who
Line 3,804: Line 3,809:
       long-period (LP) and very-long-period (VLP) volcanic seismicity; and developing
       long-period (LP) and very-long-period (VLP) volcanic seismicity; and developing
       techniques to enable the accurate identification of volcanic seismicity.'
       techniques to enable the accurate identification of volcanic seismicity.'
    professional_experience: []
    title: Volcano Seismologist

Revision as of 20:13, 30 January 2024

orcid: 

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usgs_staff_profile: 

 meta:
   url: https://www.usgs.gov/staff-profiles/phillip-dawson
   timestamp: '2024-01-30T13:13:21.706412'
   status_code: 200
 profile:
   name: Phillip Dawson, IV
   name_qualifier: null
   titles:
   - Volcano Seismologist
   organizations:
   - !!python/tuple
     - California Volcano Observatory
     - https://www.usgs.gov/observatories/calvo
   email: dawson@usgs.gov
   orcid: 0000-0003-4065-0588
   intro_statements:
   - "Phillip Dawson is a geophysicist with the U.S. Geological Survey\u2019s Volcano\
     \ Science Center, focusing on theoretical and experimental investigations of\
     \ active volcanism and volcanic processes."
   expertise_terms:
   - Volcano Seismology
   - Seismic tomography
   professional_experience: []
   education: []
   affiliations: []
   honors: []
   abstracts: []
   personal_statement: 'Phillip Dawson hails from a small town located on the flank
     of one of the worlds largest stratovolcanoes - Mount Shasta, California.  Who
     wouldnt want to pursue a career studying volcanoes at the USGS given that
     background?He currently works as a geophysicist on the Seismology of Magmatic
     Injection project at the California Volcano Observatory, Moffett Field, California.  This
     project is dedicated to understanding the underlying physics driving volcanic
     seismicity and processes through the use of detailed field experiments and the
     application, modification, and extension of existing seismic methods and theories.  Objectives
     include: quantification of volcanic velocity structure using tomography and
     surface-wave dispersion inversions; inversion of broadband waveform data to
     quantify magma transport processes; determining the effect of tilt on modern
     broadband seismic sensors, and correcting for this effect using waveform inversions;
     quantification of the effects of 3D topography and structure on seismic wave
     propagation; using dense small-aperture arrays to identify source, path, and
     site effects in tremor wavefields; quantification of the source parameters of
     long-period (LP) and very-long-period (VLP) volcanic seismicity; and developing
     techniques to enable the accurate identification of volcanic seismicity.'
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