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Nature
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Nature
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https://dx.doi.org/10.1038/188...
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Internal Waves and Waves of Sand

descriptionPublicationkeyboard_double_arrow_right Article 10 Dec 1960 English Publisher:Springer Science and Business Media LLCJournal:Nature, volume 188, pages 933-933 (issn: 0028-0836, eissn: 1476-4687, Copyright policy )
Authors: A. H. STRIDE; M. J. TUCKER;

doi: 10.1038/188933a0

Internal Waves and Waves of Sand

Abstract

A DESCRIPTION has been given of some large sand waves on La Chapelle Bank which lie parallel to the general direction of the edge of the continental shelf1. They occur within a zone about 10 miles wide, have a mean separation of 2,800 ft. and are up to 40 ft. high. Berthois2 believes them to be fossil ridges while Cartwright3 has shown in some detail how they could be formed by stationary waves, which develop in the thermocline as the tidal streams, moving landwards, feel the constraining influence of the shelf. These would be equivalent to lee-waves found on the down-wind side of a mountain.

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    popularity
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selected citations
These citations are derived from selected sources.
This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Citations provided by BIP!
popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
BIP!Popularity provided by BIP!
influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Influence provided by BIP!
impulse
This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
BIP!Impulse provided by BIP!
20
Average
Top 10%
Average
bronze