アラスカ州パブロフ火山からの火山震動と羽根の高さヒステレス
David Fee1, Matthew M Haney2, Robin S Matoza3
1Alaska Volcano Observatory, Wilson Alaska Technical Center, Geophysical Institute, University of Alaska Fairbanks, 903 Koyukuk Drive, Fairbanks, AK 99775, USA. dfee1@alaska.edu.
まとめ
2016年のパヴロフ火山の噴火は,地震の振動と灰の高さの関係が変化していることを示しました. これは火山口の侵食が 噴火の強度や排出量に影響を及ぼすことを示唆している.
科学分野:
- 地理学
- 火山学
- 音響学
背景:
- 2016年3月のパヴロフ火山の噴火は,北米の航空交通を妨害し,大きな灰を生成した.
- 地震とインフラサウンドデータは,噴火中に強い火山震動を記録した.
研究 の 目的:
- 地震の振幅と火山の噴火の高さとの関係を調べるため
- 火山噴火中の地質信号の調節における火山口の侵食の役割を調査する.
主な方法:
- EarthScope Transportable Arrayからの地震と超音波データを分析した.
- 噴火の成長と衰退の段階における震動幅と羽根の高さの比較.
主要な成果:
- 震動の振幅と羽根の高さの間の変数関係が観察され,ヒステリシスを示した.
- このヒステレシスは,火山口の不可逆的な構造変化を示唆し,おそらく侵食によるものです.
結論:
- 火山噴出孔の侵食は,地震の振動と噴火のダイナミクスの関係に大きな影響を与えます.
- この関係を理解することで,火山の放射能の推定と噴火の特徴を高めることができます.
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