Abstract

The U.S. Geological Survey (USGS) “Did You Feel It?” (DYFI) system is an automated approach for rapidly collecting macroseismic intensity data from Internet users’ shaking and damage reports and generating intensity maps immediately following earthquakes; it has been operating for over a decade (1999-2011). DYFI-based intensity maps made rapidly available through the DYFI system fundamentally depart from more traditional maps made available in the past. The maps are made more quickly, provide more complete coverage and higher resolution, provide for citizen input and interaction, and allow data collection at rates and quantities never before considered. These aspects of Internet data collection, in turn, allow for data analyses, graphics, and ways to communicate with the public, opportunities not possible with traditional data-collection approaches. Yet web-based contributions also pose considerable challenges, as discussed herein. After a decade of operational experience with the DYFI system and users, we document refinements to the processing and algorithmic procedures since DYFI was first conceived. We also describe a number of automatic post-processing tools, operations, applications, and research directions, all of which utilize the extensive DYFI intensity datasets now gathered in near-real time. DYFI can be found online at the website http://earthquake.usgs.gov/dyfi/.

Highlights

  • Over the past decade, the U.S Geological Survey’s “Did You Feel It?®” (DYFI) system has automatically collected shaking and damage reports from Internet users immediately following earthquakes

  • Worden et al [2011] detail the process and uncertainties associated with directly transforming DYFI intensity to peak ground motion estimates, but based on the repeatability seen with these data, we consider that process to be informative for a number of real-time (ShakeMap and magnitude determinations) and other seismological analyses

  • DYFI reports of sonic booms provide quantitative data for long-observed characteristics that are diagnostic of the phenomena: spatially and temporally correlated lowintensity reports from a rather broad geographic area, the lack of an associated instrumentally recorded earthquake that is large enough to be felt over the area from which reports are received, and the nature of user entries: rattled windows are noted nearly ubiquitously in the response or comments provided

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Summary

Introduction

The U.S Geological Survey’s “Did You Feel It?®” (DYFI) system has automatically collected shaking and damage reports from Internet users immediately following earthquakes. DYFI is a rapid and vast source of macroseismic data, providing quantitative and qualitative information about shaking intensities for earthquakes in the USA and around the globe.

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