Abstract
OSBORNE REYNOLDS, in a short paper entitled “On the Action of Rain to Calm the Sea"1, discussed the action of rain in calming a rough sea. He expressed the opinion that each drop of rain produces a vortex ring which, on descending into the water, transfers momentum from the surface layers to the underneath layers, thus reducing the relative motion of the layers. It was suggested to us by Prof. A. H. Gibson that further experiments were desirable to confirm the above theory.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on SpringerLink
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
References
Reynolds, O., “Papers Mechanical and Physical Subjects", 86 (Camb. Univ. Press).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
ASHTON, E., O'SULLIVAN, J. Effect of Rain in Calming the Sea. Nature 164, 320–321 (1949). https://doi.org/10.1038/164320a0
Issue date:
DOI: https://doi.org/10.1038/164320a0
This article is cited by
-
Effect of Rain in Calming the Sea
Nature (1950)