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GRAVITY INDUCED DISPERSION FOR NEARLY FLAT VORTEX SHEETS
Conference proceeding

GRAVITY INDUCED DISPERSION FOR NEARLY FLAT VORTEX SHEETS

Daniel Spirn and J. Douglas Wright
PROCEEDINGS OF THE CONFERENCE ON WATER WAVES: THEORY AND EXPERIMENT, pp.1-6
01 Jan 2010

Abstract

Engineering Engineering, Ocean Oceanography Physical Sciences Science & Technology Technology
Using techniques from the theory of oscillatory integrals, we prove rigorous estimates which show that the linearization of the vortex sheet equations of motion about a quiescent state disperse under certain circumstances. Such dispersion is only possible only through the joint effects of surface tension (which damps high frequency modes) and gravitation (which damps low frequency modes).

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Collaboration types
Domestic collaboration
Web of Science research areas
Engineering, Ocean
Oceanography