Ice Vibrations on the Arctic Channel.
Differences in signal-to-noise ratios between hydrophones and geophones were measured as a function of signal grazing angle with level ice and signal frequency. The frequency distributions in the differences clearly show two groupings. One group represents waves traveling in the Arctic sound channel...
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Format: | Text |
Language: | English |
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1996
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Online Access: | http://www.dtic.mil/docs/citations/ADA317278 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA317278 |