Abstract

In this paper we consider two model systems of equations obtained by taking the Hodge duals of the Euler and the Navier–Stokes systems, respectively. The ‘vorticity’ formulation of the new system becomes a nonlinear, non-local scalar equation having similarities to the quasi-geostrophic equations. We prove the local existence of classical solutions, and derive the Beale-Kato-Majda type of blow-up criterion for the dual Euler system. Moreover, we actually show that the finite-time blow-up occurs for generic non-trivial initial data for this system. For the dual Navier-Stokes equations we construct an explicitly global-in-time smooth solution for general initial data, using the Hopf-Cole transform. In the appendix we formulate the Euler system and the dual Euler system in terms of the Clifford algebra.

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.