Morgan P. Moschetti

Morgan P. Moschetti

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Morgan P. Moschetti

U.S. Geological Survey Golden Colorado USA

Research Focus & Metrics

Academic Career Length

20Years (2007-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 June 2007 in Geophysical Journal International
Verified
Journal Article
Open access
PDF file
GBG. D. Bensen
G. D. Bensen
MRM. H. Ritzwoller
M. H. Ritzwoller
MBM. P. Barmin
M. P. Barmin
ALA. L. Levshin
A. L. Levshin
FLF. Lin
F. Lin
YYY. Yang
Y. Yang
Summary. Ambient noise tomography is a rapidly emerging field of seismological research. This paper presents the current status of ambient noise data processin

1 April 2008 in Geophysical Journal International
Verified
Journal Article
Open access
PDF file
FLFan-Chi Lin
Fan-Chi Lin
MMMorgan P. Moschetti
Morgan P. Moschetti
MRMichael H. Ritzwoller
Michael H. Ritzwoller
Summary. We present the results of Rayleigh wave and Love wave phase velocity tomography in the western United States using ambient seismic noise observed at o

1 January 2014
Verified
Report
Closed access
MPMark D. Petersen
Mark D. Petersen
MMMorgan P. Moschetti
Morgan P. Moschetti
PPPeter M. Powers
Peter M. Powers
CMCharles S. Mueller
Charles S. Mueller
KHKathleen M. Haller
Kathleen M. Haller
AOAnna H. Olsen
Anna H. Olsen

8 April 2010 in Nature
Verified
Journal Article
Closed access
MMM. P. Moschetti
M. P. Moschetti
MRM. H. Ritzwoller
M. H. Ritzwoller
FLF. Lin
F. Lin
YYY. Yang
Y. Yang

21 August 2007 in Geochemistry, Geophysics, Geosystems
Verified
Journal Article
Closed access
PDF file
MMM. P. Moschetti
M. P. Moschetti
MRM. H. Ritzwoller
M. H. Ritzwoller
NSN. M. Shapiro
N. M. Shapiro

1 February 2024 in Earthquake Spectra
Verified
Journal Article
Open access
MPMark D Petersen
Mark D Petersen
ASAllison M Shumway
Allison M Shumway
PPPeter M Powers
Peter M Powers
EFEdward H Field
Edward H Field
MMMorgan P Moschetti
Morgan P Moschetti
RWRobert C Witter
Robert C Witter
The US National Seismic Hazard Model (NSHM) was updated in 2023 for all 50 states using new science on seismicity, fault ruptures, ground motions, and probabilistic techniques to produce a standard of practice for public policy and other engineering applications (defined for return periods greater than ∼475 or less than ∼10,000 years). Changes in 2023 time‐independent seismic hazard (both increases and decreases compared to previous NSHMs) are substantial because the new model considers more data and updated earthquake rupture forecasts and ground‐motion components. In developing the 2023 model, we tried to apply best available or applicable science based on advice of co‐authors, more than 50 reviewers, and hundreds of hazard scientists and end‐users, who attended public workshops and provided technical inputs. The hazard assessment incorporates new catalogs, declustering algorithms, gridded seismicity models, magnitude‐scaling equations, fault‐based structural and deformation models, multi‐fault earthquake rupture forecast models, semi‐empirical and simulation‐based ground‐motion models, and site amplification models conditioned on shear‐wave velocities of the upper 30 m of soil and deeper sedimentary basin structures. Seismic hazard calculations yield hazard curves at hundreds of thousands of sites, ground‐motion maps, uniform‐hazard response spectra, and disaggregations developed for pseudo‐spectral accelerations at 21 oscillator periods and two peak parameters, Modified Mercalli Intensity, and 8 site classes required by building codes and other public policy applications. Tests show the new model is consistent with past ShakeMap intensity observations. Sensitivity and uncertainty assessments ensure resulting ground motions are compatible with known hazard information and highlight the range and causes of variability in ground motions. We produce several impact products including building seismic design criteria, intensity maps, planning scenarios, and engineering risk assessments showing the potential physical and social impacts. These applications provide a basis for assessing, planning, and mitigating the effects of future earthquakes.