التفاصيل البيبلوغرافية
| العنوان: |
Meteoroid studies on DAS and large-N networks: data sets |
| المؤلفون: |
Vera Rodriguez, Ismail, Isken, Marius P., Dahm, Torsten, Jousset, Philippe, Lamb, Oliver D., Kristjánsdóttir, Sigríður, Jónsdóttir, Kristín, Sanchez-Pastor, Pilar, Clinton, John, Wollin, Christopher, Baird, Alan F., Wuestefel, Andreas, Eibl, Eva P. S., Goertz-Allmann, Bettina P., Oye, Volker, Hjörleifsdóttir, Vala, Obermann, Anne, Kraft, Toni |
| المساهمون: |
Jousset, Philippe, Vera-Rodriguez, Ismail |
| بيانات النشر: |
GFZ Data Services |
| سنة النشر: |
2022 |
| المجموعة: |
GFZ Data Services (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
| مصطلحات موضوعية: |
Large-N seismometers networks, Distributed fibre optic sensing, EARTH SCIENCE > SOLID EARTH > ROCKS/MINERALS/CRYSTALS > METEORITES, EARTH SCIENCE > SOLID EARTH > ROCKS/MINERALS/CRYSTALS > METEORITES > METEORITE ORIGIN |
| جغرافية الموضوع: |
23 -20 63.7 64.4 |
| Time: |
Southwest Iceland 02-07-2022 |
| الوصف: |
We present an outstanding record of local, dense Large-N seismic and distributed acoustic sensor observations of a meteoroid from July 2, 2021 in Iceland. Our dataset includes high-quality observations from seven small aperture arrays of few hundred meters, an infrasound array, and a rotational station, all located within the distance range of 300 km. The high-frequency data show a variety of different phases associated with the source process along the atmospheric trajectory, including impulsive negative 1 first ground motions, a complex coda wave train about 2.5 s long thereafter, an azimuth-dependent stopping phase with reversed polarity between 1-25 s after the first arrival, which is resolved over only a few kilometers. The ground motion amplitude between the first and last arrivals is generally elevated. We associate the waveform in the 2.5 s coda with meteor-atmosphere interactions and nonlinear plasma processes that produce an oscillating shock-wave source pulse. Our data suggest a small azimuth-dependent deflection or dispersion of this source pulse, which may be related to the meteoroid’s deceleration in the atmosphere. We present a finite-length kinematic line-source pulse model that consistently explains the different phases inside and outside the Mach cone segment of our images, their wave amplitude variations, and a polarity change between the first phase and the terminating phase. The previously undiscovered rich directivity effects can also explain seemingly contradictory, time-dependent wave energy beam-directions at the various small aperture arrays and along the DAS cable. A combination of conventional locations and a Bayesian inversion of first and stopping phase arrivals led to a precise localization of the meteor trajectory. |
| نوع الوثيقة: |
dataset |
| اللغة: |
unknown |
| Relation: |
http://dx.doi.org/10.5880/GFZ.2.2.2022.002 |
| DOI: |
10.5880/GFZ.2.2.2022.002 |
| الاتاحة: |
https://doi.org/10.5880/GFZ.2.2.2022.002 |
| Rights: |
CC BY 4.0 ; http://creativecommons.org/licenses/by/4.0/ |
| رقم الانضمام: |
edsbas.79D1616 |
| قاعدة البيانات: |
BASE |