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Turbulence and jet-driven zonal flows: Secondary circulation in rotating fluids due to asymmetric forcing.
Burin, M J; Caspary, K J; Edlund, E M; Ezeta, R; Gilson, E P; Ji, H; McNulty, M; Squire, J; Tynan, G R.
Afiliación
  • Burin MJ; Department of Physics, California State University San Marcos, San Marcos, California 92096, USA.
  • Caspary KJ; Princeton Plasma Physics Laboratory, Princeton University, Princeton, New Jersey 08544, USA.
  • Edlund EM; Department of Physics, State University of New York College at Cortland, Cortland, New York 13045, USA.
  • Ezeta R; Max Planck Center for Complex Fluid Dynamics, Mesa+ Institute, and J. M. Burgers Centre for Fluid Dynamics, University of Twente, P.O. Box 217, 7500AE Enschede, The Netherlands.
  • Gilson EP; Princeton Plasma Physics Laboratory, Princeton University, Princeton, New Jersey 08544, USA.
  • Ji H; Department of Astrophysical Sciences and Princeton Plasma Physics Laboratory, Princeton University, Princeton, New Jersey 08544, USA.
  • McNulty M; Department of Mathematics, University of California Riverside, Riverside, California 92521, USA.
  • Squire J; Department of Physics, University of Otago, Dunedin 9016, New Zealand and Theoretical Astrophysics, California Institute of Technology, Pasadena, California 91125, USA.
  • Tynan GR; Department of Mechanical Engineering and the Center for Energy Research, Jacobs School of Engineering, University of California, San Diego 92093, USA.
Phys Rev E ; 99(2-1): 023108, 2019 Feb.
Article en En | MEDLINE | ID: mdl-30934347
We report on experiments and modeling on a rotating confined liquid that is forced by circumferential jets coaxial with the rotation axis, wherein system-scale secondary flows are observed to emerge. The jets are evenly divided in number between inlets and outlets and have zero net mass transport. For low forcing strengths the sign of this flow depends on the sign of a sloped end cap, which simulates a planetary ß plane. For increased forcing strengths the secondary flow direction is insensitive to the slope sign, and instead appears to be dominated by an asymmetry in the forcing mechanism, namely, the difference in radial divergence between the inlet and outlet jet profiles. This asymmetry yields a net radial velocity that is affected by the Coriolis force, inducing secondary zonal flow.

Texto completo: 1 Colección: 01-internacional Banco de datos: MEDLINE Idioma: En Revista: Phys Rev E Año: 2019 Tipo del documento: Article País de afiliación: Estados Unidos

Texto completo: 1 Colección: 01-internacional Banco de datos: MEDLINE Idioma: En Revista: Phys Rev E Año: 2019 Tipo del documento: Article País de afiliación: Estados Unidos