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1000 Titel
  • The 12 December 2017 Baumgarten Gas Hub Explosion: A Case Study on Understanding the Occurrence of a Large Infrasound Azimuth Residual and a Lack of Seismic Observations
1000 Autor/in
  1. Koch, Karl |
  2. Pilger, Christoph |
  3. Czanik, Csenge |
  4. Bondár, István |
1000 Erscheinungsjahr 2020
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2020-07-27
1000 Erschienen in
1000 Quellenangabe
  • 177(10):4957-4970
1000 Copyrightjahr
  • 2020
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.1007/s00024-020-02549-2 |
1000 Publikationsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:title>Abstract</jats:title><jats:p>The Baumgarten explosion occurred on 12 December 2017 at a gas storage site about 30 km east of Vienna, Austria. Acoustic arrivals from this accidental surface explosion were detected at dozens of stations of the AlpArray seismic network to distances up to 150 km, mainly in easterly directions. Thus it was expected that the Hungarian infrasound array PSZI located about 230 km to the east-southeast of Baumgarten would detect this acoustic wave as well. Standard progressive multichannel correlation processing and frequency-wavenumber analysis identified a signal emerging at 7:57:55 UTC from an azimuth of 296°–300° and with trace-velocity &gt; 400 m/s. The extraordinarily high trace-velocity and excessive backazimuth residual, relative to the explosion site direction of 282°, however cast strong doubts on the arrival’s connection to the Baumgarten event. Accounting for the effect of non-planar geometry of the infrasound array results in a reduction of the azimuth residual by half. Additionally, 2D and 3D raytracing methods are used including the European Centre for Medium-Range Weather Forecasts (ECMWF) atmospheric model to further explain the remaining azimuth residual as well as to elucidate the large trace velocity estimates. The prevailing stratospheric winds in excess of 150 m/s are identified as the underlying cause. Including both factors the initial azimuth residual of up to 18° decreases to ~ 4°, allowing to associate the infrasound signal at PSZI with the Baumgarten event. Finally, the data from a seismic station at 30 km range is re-investigated for magnitude estimation. The local magnitude of M<jats:sub>L</jats:sub> &lt; 1.0 explains well the scarcity of seismic observations within 50 km range, where three or four stations show signals, mainly consisting of Rg-type surface waves, but no body waves.</jats:p>
1000 Sacherschließung
lokal Article
lokal array data processing
lokal atmospheric sound propagation
lokal detection threshold
lokal Baumgarten explosion
lokal backazimuth residual
lokal Infrasound
1000 Liste der Beteiligten
  1. https://orcid.org/0000-0001-7101-5419|https://frl.publisso.de/adhoc/uri/UGlsZ2VyLCBDaHJpc3RvcGg=|https://frl.publisso.de/adhoc/uri/Q3phbmlrLCBDc2VuZ2U=|https://frl.publisso.de/adhoc/uri/Qm9uZMOhciwgSXN0dsOhbg==
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