Felt Reports for Rapid Mapping of Global Earthquake Damage: The Doughnut Effect?

Abstract

Research Article| December 06, 2017 Felt Reports for Rapid Mapping of Global Earthquake Damage: The Doughnut Effect? Rémy Bossu; Rémy Bossu aEuropean‐Mediterranean Seismological Centre, c/o CEA, 91297 Arpajon Cedex, France, [e-mail] at CEA, DAM, DIF, F‐91297 Arpajon, France. Search for other works by this author on: GSW Google Scholar Matthieu Landès; Matthieu Landès aEuropean‐Mediterranean Seismological Centre, c/o CEA, 91297 Arpajon Cedex, France, [e-mail] Search for other works by this author on: GSW Google Scholar Frédéric Roussel; Frédéric Roussel aEuropean‐Mediterranean Seismological Centre, c/o CEA, 91297 Arpajon Cedex, France, [e-mail] Search for other works by this author on: GSW Google Scholar Robert Steed Robert Steed aEuropean‐Mediterranean Seismological Centre, c/o CEA, 91297 Arpajon Cedex, France, [e-mail] Search for other works by this author on: GSW Google Scholar Seismological Research Letters (2018) 89 (1): 138–144. https://doi.org/10.1785/0220170129 Article history first online: 06 Dec 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Rémy Bossu, Matthieu Landès, Frédéric Roussel, Robert Steed; Felt Reports for Rapid Mapping of Global Earthquake Damage: The Doughnut Effect?. Seismological Research Letters 2017;; 89 (1): 138–144. doi: https://doi.org/10.1785/0220170129 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search ABSTRACT Thanks to the Internet and mobile technologies, the collection of felt reports after global earthquakes is today remarkably efficient and rapid. Despite the volume of collected reports, it remains unclear whether felt reports on their own can provide a complete and rapid picture of earthquake's effects, especially for damaging shaking levels. To answer this question, we analyze the response rates and time characteristics of 55,000 felt reports collected at the European‐Mediterranean Seismological Centre (EMSC) and 120,000 launches of its LastQuake smartphone application within an hour of the 108 global earthquakes studied. The number of reports corresponding to damaging shaking levels (intensity 7 and above) is very limited and, if any, they are collected much later than lower intensity level reports. Intensities 5–6 level reports are collected in significant numbers but typically 20 min after lower intensities. The application launches that benefit from having precise locations share similar variations in time and intensity levels as felt reports. First, we conclude that felt reports alone without their temporal characteristics are unlikely to rapidly provide a full and complete picture of damage related to global earthquakes. However, there is a general schematic pattern for data collected by EMSC named the doughnut effect in which damaged zones are free of felt reports and ultimately surrounded by intensities 5–6. This pattern is not a proof of damage but can be helpful to identify zones potentially affected by severe damage. For earthquakes with maximum intensities 5–6, the initial doughnut shape observed immediately after the earthquake rapidly disappears (about 20 min) as intensities 5 and 6 reports get shared by eyewitnesses. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.