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dc.contributor.author
Chung, Angela, I
dc.contributor.author
Meier, Men-Andrin
dc.contributor.author
Andrews, Jennifer
dc.contributor.author
Böse, Maren
dc.contributor.author
Crowell, Brendan W.
dc.contributor.author
McGuire, Jeffrey J.
dc.contributor.author
Smith, Deborah E.
dc.date.accessioned
2020-09-03T15:33:31Z
dc.date.available
2020-08-27T02:51:26Z
dc.date.available
2020-09-03T15:33:31Z
dc.date.issued
2020-08-01
dc.identifier.issn
0037-1106
dc.identifier.issn
1943-3573
dc.identifier.other
10.1785/0120200032
en_US
dc.identifier.uri
http://hdl.handle.net/20.500.11850/432793
dc.description.abstract
During July 2019, a sequence of earthquakes, including an Mw 6.4 foreshock and an Mw 7.1 mainshock, occurred near Ridgecrest, California. ShakeAlert, the U.S. Geological Survey (USGS) earthquake early warning system being developed for the U.S. West Coast, was operational during this time, although public alerting was only available within Los Angeles County. ShakeAlert created alert messages for the two largest events and for many of the larger aftershocks. In this study, we dissect log files and replay data through the system to reconstruct the sequence of events and analyze the performance of the system during that period. Although the system performed reasonably well overall, the sequence also revealed various issues and short comings that will be addressed in impend-ing and future system upgrades. ShakeAlert detected and characterized both the Mw 6.4 and Mw 7.1 earthquakes within 6.9 s of their origin times and created alert messages that were available to ShakeAlert’s pilot users. No public alerts were sent out by the ShakeAlertLA cell phone app (the only publicly available alerting method at the time), because the predicted shaking for Los Angeles County was below the app’s alerting thresh-old of modified Mercalli intensity 4.0. For the Mw 6.4 event, this was accurate. For the Mw 7.1 event, public alerts for Los Angeles County were warranted, but ShakeAlert under-predicted the shaking levels, because both the point-source and finite-fault algorithms underestimated the magnitude of the earthquake by 0.8 units. A number of software and hardware issues that were responsible for the magnitude underestimation of the mainshock have been identified and will be addressed in future ShakeAlert releases. We also analyze the hypothetical alerting performance of ShakeAlert had public alerting been available throughout southern California. © Seismological Society of America.
en_US
dc.language.iso
en
en_US
dc.publisher
Seismological Society of America
en_US
dc.title
ShakeAlert Earthquake Early Warning System Performance during the 2019 Ridgecrest Earthquake Sequence
en_US
dc.type
Journal Article
dc.date.published
2020-07-21
ethz.journal.title
Bulletin of the Seismological Society of America
ethz.journal.volume
110
en_US
ethz.journal.issue
4
en_US
ethz.journal.abbreviated
Bull. Seismo. Soc. Am.
ethz.pages.start
1904
en_US
ethz.pages.end
1923
en_US
ethz.identifier.wos
ethz.identifier.scopus
ethz.publication.place
Albany, CA
en_US
ethz.publication.status
published
en_US
ethz.leitzahl
ETH Zürich::00002 - ETH Zürich::00003 - Schulleitung und Dienste::00022 - Bereich VP Forschung / Domain VP Research::02818 - Schweiz. Erdbebendienst (SED) / Swiss Seismological Service (SED)
ethz.leitzahl.certified
ETH Zürich::00002 - ETH Zürich::00003 - Schulleitung und Dienste::00022 - Bereich VP Forschung / Domain VP Research::02818 - Schweiz. Erdbebendienst (SED) / Swiss Seismological Service (SED)
ethz.date.deposited
2020-08-27T02:51:30Z
ethz.source
WOS
ethz.eth
yes
en_US
ethz.availability
Metadata only
en_US
ethz.rosetta.installDate
2020-09-03T15:33:41Z
ethz.rosetta.lastUpdated
2022-03-29T03:03:14Z
ethz.rosetta.versionExported
true
ethz.COinS
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