摘要 : Noise with periods 3 to 10 s, ubiquitous in seismic records, is expected to be mostly generated by pairs of ocean wave trains of opposing propagation directions with half the seismic frequency. Here we present the first comprehens... 展开
作者 | Fabrice Ardhuin Eleonore Stutzmann Martin Schimmel Anne Mangeney |
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作者单位 | |
期刊名称 | 《Journal of Geophysical Research, C. Oceans: JGR》 |
总页数 | 21 |
语种/中图分类号 | 英语 / P3 |
关键词 | Ocean sources noise |
馆藏号 | N2008EPST0000392 |