We compute time-periodic solutions of a simple model for the vortex sheet with surface tension. The model has the same dispersion relation as the full system of evolution equations, and it also has the same destabilizing nonlinearity (if the surface tension parameter were to be set to zero, then this nonlinearity would cause an analogue of the Kelvin-Helmholtz instability). The numerical method uses a gradient descent algorithm to minimize a functional which measures whether a solution of the system is time periodic. We find continua of genuinely time-periodic solutions bifurcating from equilibrium.
COMPUTING TIME-PERIODIC SOLUTIONS OF A MODEL FOR THE VORTEX SHEET WITH SURFACE TENSION
Creators
David M. Ambrose - Drexel University
Mark Kondrla - Drexel University
Michael Valle - Drexel University
Publication Details
Quarterly of applied mathematics, v 73(2), pp 317-329
Publisher
Brown Univ
Number of pages
13
Grant note
Drexel University Office of the Provost
DMS-1008387; DMS-1016267 / National Science Foundation through NSF; National Science Foundation (NSF)
Steinbright Career Development Office
Resource Type
Journal article
Language
English
Academic Unit
Mathematics
Web of Science ID
WOS:000370801800005
Scopus ID
2-s2.0-84930852548
Other Identifier
991019170399804721
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