Estimation of Seismic Attenuation of the Greenland Ice Sheet Using 3-D Waveform Modeling

Genti Toyokuni, Masanao Komatsu, Hiroshi Takenaka

研究成果: Article査読

抄録

We estimated the seismic attenuation (Q factor) of the Greenland Ice Sheet (GrIS) by comparing observed and theoretical Rayleigh waveforms. Observed waveforms are obtained by interfering noise waveforms in vertical-component seismograms between stations belonging to the latest broadband seismic network distributed throughout Greenland (GLISN network). Theoretical waveforms are calculated by parallel computation using the latest 3-D seismic waveform modeling method. Comparing the observed waveforms with the theoretical waveforms at different Q factors reveals that the GrIS has a low Q of 10 ≤ QP, QS ≤ 50, indicating very high attenuation of seismic waves due to the ice. This study is the first to establish the low Q factor of ice sheets via ultra-long-distance propagation (350−1,000 km). The Q factors obtained in this study are indispensable for estimating the thermal state and density distribution of the GrIS, as well as for interpreting the characteristics of seismic waveform that propagates through the GrIS.

本文言語English
論文番号e2021JB021694
ジャーナルJournal of Geophysical Research: Solid Earth
126
4
DOI
出版ステータスPublished - 2021 4

ASJC Scopus subject areas

  • 地球物理学
  • 地球化学および岩石学
  • 地球惑星科学(その他)
  • 宇宙惑星科学

フィンガープリント

「Estimation of Seismic Attenuation of the Greenland Ice Sheet Using 3-D Waveform Modeling」の研究トピックを掘り下げます。これらがまとまってユニークなフィンガープリントを構成します。

引用スタイル