A magnetic anomaly and particle velocity array correlator for the detection of internal waves in the ocean
Related literature has shown that internal waves (IWs) observed in the ocean are capable of producing secondary magnetic fields with a small signal-to-noise ratio due to the flow of dissolved salts. It can be difficult to characterize these signals since they are relatively weak, highly transient, a...
| Príomhchruthaitheoirí: | , , , |
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| Formáid: | Alt |
| Teanga: | English |
| Foilsithe / Cruthaithe: |
AIP Publishing LLC
2024-07-01
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| Sraith: | AIP Advances |
| Rochtain ar líne: | http://dx.doi.org/10.1063/5.0207529 |