<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Liam Toney</dc:contributor>
  <dc:contributor>Keehoon Kim</dc:contributor>
  <dc:contributor>Richard Sanderson</dc:contributor>
  <dc:contributor>Alexandra M. Iezzi</dc:contributor>
  <dc:contributor>Robin S Matoza</dc:contributor>
  <dc:contributor>Silvio DeAngelis</dc:contributor>
  <dc:contributor>Art Jolly</dc:contributor>
  <dc:contributor>John J. Lyons</dc:contributor>
  <dc:contributor>Matthew M. Haney</dc:contributor>
  <dc:creator>David Fee</dc:creator>
  <dc:date>2021</dc:date>
  <dc:description>&lt;div class="JournalAbstract"&gt;&lt;p class="mb15"&gt;Infrasound data are routinely used to detect and locate volcanic and other explosions, using both arrays and single sensor networks. However, at local distances (&amp;lt;15 km) topography often complicates acoustic propagation, resulting in inaccurate acoustic travel times leading to biased source locations when assuming straight-line propagation. Here we present a new method, termed Reverse Time Migration-Finite-Difference Time Domain (RTM-FDTD), that integrates numerical modeling into the standard RTM back-projection process. Travel time information is computed across the entire potential source grid via FDTD modeling to incorporate the effects of topography. The waveforms are then back-projected and stacked at each grid point, with the stack maximum corresponding to the likely source. We apply our method to three volcanoes with different network configurations, source-receiver distances, and topography. At Yasur Volcano, Vanuatu, RTM-FDTD locates explosions within ∼20 m of the source and differentiates between multiple vents. RTM-FDTD produces a more accurate location for the two Yasur subcraters than standard RTM and doubles the number of detected events. At Sakurajima Volcano, Japan, RTM-FDTD locates the source within 50 m of the active vent despite notable topographic blocking. The RTM-FDTD location is similar to that from the Time Reversal Mirror method, but is more computationally efficient. Lastly, at Shishaldin Volcano, Alaska, RTM and RTM-FDTD both produce realistic source locations (&amp;lt;50 m) for ground-coupled airwaves recorded on a four-station seismic network. We show that RTM is an effective method to detect and locate infrasonic sources across a variety of scenarios, and by integrating numerical modeling, RTM-FDTD produces more accurate source locations and increases the detection capability.&lt;/p&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3389/feart.2021.620813</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Frontiers</dc:publisher>
  <dc:title>Local explosion detection and infrasound localization by reverse time migration using 3-D finite-difference wave propagation</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>