II. On the formation of coreless vortices by the motion of a solid through an inviscid incompressible fluid
Author(s) -
William Thomson
Publication year - 1887
Publication title -
proceedings of the royal society of london
Language(s) - English
Resource type - Journals
eISSN - 2053-9126
pISSN - 0370-1662
DOI - 10.1098/rspl.1887.0018
Subject(s) - globe , inviscid flow , compressibility , mechanics , equator , vortex , physics , geology , geodesy , medicine , ophthalmology , latitude
Take the simplest case: let the moving solid be a globe, and let the fluid be of infinite extent in all directions. Let its pressure be of any given value, P, at infinite distances from the globe, and let the globe be kept moving with a given constant velocity, V. If the fluid keeps everywhere in contact with the globe, its velocity relatively to the globe at the equator (which is the place of greatest relative velocity) is 3/2 V. Hence, unless P> 5/8 V2 , the fluid will not remain in contact with the globe.
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