Item talk:Q272171
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{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Real-time earthquake detection and alerting behavior of PLUM ground-motion-based early warning in the United States", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70237103", "url": "https://pubs.usgs.gov/publication/70237103" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70237103 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1785/0120220022", "url": "https://doi.org/10.1785/0120220022" } ], "journal": { "@type": "Periodical", "name": "Bulletin of the Seismological Society of America", "volumeNumber": "112", "issueNumber": "5" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Bulletin of the Seismological Society of America" } ], "datePublished": "2022", "dateModified": "2022-09-29", "abstract": "We examine the real\u2010time earthquake detection and alerting behavior of the Propagation of Local Undamped Motion (PLUM) earthquake early warning (EEW) algorithm and compare PLUM\u2019s performance with the real\u2010time performance of the current source\u2010characterization\u2010based ShakeAlert System. In the United States (U.S.), PLUM uses a two\u2010station approach to detect earthquakes. Once a detection is confirmed, observed modified Mercalli intensity (MMI) distributions are forecast onto a regular grid, in which the preferred alert regions are grid cells with MMI 4.0+ forecasts. Although locations of dense station coverage allow PLUM to detect small (M\u00a0< 4.5) earthquakes typically not considered for EEW in the U.S., a PLUM detection on a small earthquake does not always generate an alert. This is because PLUM alerts are determined by current shaking distributions. If the MMI 4.0+ shaking subsides prior to detection confirmation by shaking at a second neighboring station, the prior MMI 4.0+ information will not be in the alert forecasts. Of the 432\u00a0M\u00a03.0+ U.S. West Coast earthquakes in 2021, 33 produced ground motions large enough to be detected by PLUM. Twenty\u2010four generated MMI 4.0+ PLUM alerts, whereas ShakeAlert issued public EEW alerts for 13 of these earthquakes. We compare PLUM and ShakeAlert alert regions with ShakeMap and \u201cDid You Feel It?\u201d intensity distributions. Because PLUM alert regions surround stations observed to have strong ground motions (regardless of earthquake magnitude), PLUM alerts reliably include locations that experience significant shaking. This is not necessarily the case for ShakeAlert alert regions when there are large errors in magnitude or epicenter estimates. For two of the largest earthquakes in our real\u2010time dataset, the\u00a0M\u00a06.0 Antelope Valley and\u00a0M\u00a05.1 Petrolia earthquakes, the inclusion of PLUM would have improved real\u2010time ShakeAlert performance. Our results indicate that incorporation of PLUM into ShakeAlert will improve the robustness of the EEW system.", "description": "21 p.", "publisher": { "@type": "Organization", "name": "Seismological Society of America" }, "author": [ { "@type": "Person", "name": "Saunders, Jessie Kate", "givenName": "Jessie Kate", "familyName": "Saunders", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-5340-6715", "url": "https://orcid.org/0000-0001-5340-6715" }, "affiliation": [ { "@type": "Organization", "name": "Earthquake Science Center", "url": "https://www.usgs.gov/centers/earthquake-science-center" } ] }, { "@type": "Person", "name": "Minson, Sarah E. sminson@usgs.gov", "givenName": "Sarah E.", "familyName": "Minson", "email": "sminson@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-5869-3477", "url": "https://orcid.org/0000-0001-5869-3477" }, "affiliation": [ { "@type": "Organization", "name": "Earthquake 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