Experimental observation of swirl accumulation in a magnetically driven flow

作者：I. Grants, Chengyi Zhang, Sven Eckert, G. Gerbeth · 发表于：Journal of Fluid Mechanics · 年份：2008 · DOI：10.1017/s0022112008003650 · 被引用次数：33 · 研究领域：Tropical and Extratropical Cyclones Research、Solar and Space Plasma Dynamics、Meteorological Phenomena and Simulations

Independent poloidal and azimuthal body forces are induced in a liquid metal cylinder by travelling and rotating magnetic fields of different frequencies, respectively. The bulk axial and azimuthal velocities are measured by the ultrasound Doppler method. Particle image velocimetry is used to observe the upper free surface velocity distribution. The transition from the poloidal to the azimuthal body force governed regime occurs at a fixed ratio of the respective force magnitude of around 100. This transition is marked by the formation of a concentrated vortex revealing several similarities to intense atmospheric vortices. The vortex structure is controlled by a relatively weak azimuthal force while the maximum speed of the swirl is mainly governed by the poloidal one. Under a certain force ratio the average axial velocity changes its direction in the vortex core, resembling the subsidence in an eye of a tropical cyclone or a large tornado. Multiple moving vortices encircle the vortex core in this regime.