衰减
宽带
地震学
地质学
地震噪声
噪音(视频)
声学
电信
工程类
光学
物理
计算机科学
图像(数学)
人工智能
作者
C. R. Hutt,Adam T. Ringler,L. S. Gee
摘要
Abstract Seismic noise induced by atmospheric processes such as wind and pressure changes can be a major contributor to the background noise observed in many seismograph stations, especially those installed at or near the surface. Cultural noise such as vehicle traffic or nearby buildings with air handling equipment also contributes to seismic background noise. Such noise sources fundamentally limit our ability to resolve earthquake‐generated signals. Many previous seismic noise versus depth studies focused separately on either high‐frequency (>1 Hz) or low‐frequency (
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