Physical Sources of High‐Frequency Seismic Noise on Cascadia Initiative Ocean Bottom Seismometers
Abstract Physical sources of high‐frequency seismic noise in the ocean are investigated using data from the Cascadia Initiative (CI) ocean bottom seismometer (OBS) network, hindcasts of wind speed, waves, and the bottom currents predicted by a regional ocean circulation model and observed at sites o...
I tiakina i:
| Ngā kaituhi matua: | , |
|---|---|
| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
Wiley
2020-10-01
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| Rangatū: | Geochemistry, Geophysics, Geosystems |
| Ngā marau: | |
| Urunga tuihono: | https://doi.org/10.1029/2020GC009085 |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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