Sentence examples for circulation vortex from inspiring English sources

The circulation vortex then transports the soot from the interior of the recirculation zone toward less rich mixture fractions near the flame, which is situated in the outer shear layer between the air coflow and the recirculation zone.

If the circulation of the vortex moves around the northern tip of Taiwan, it can induce a significant secondary vortex on the lee side.

Second, the tip vortex circulation is calculated based on the converged wake shape and doublet distribution.

Available knowledge indicates that this points to a rather strong vortex circulation and related strong and persistent main flow velocity.

We find that the circulation around the vortex scours gas from the preheat zone in front of the flame, making the interaction sensitive to equivalence ratio.

Clockwise and counter-clockwise rotating streamwise vortices are sampled and the probability density function of the vortex circulation Reynolds number and wall Nusselt number are calculated.

It is concluded that the estimated optimal tube diameters and entrance length of the header can indeed effectively eliminate the eddy flow in the first tube due to the circulation of the vortex flow near the header inlet.

The numerical results reveal that 50% reduction of the wake dissipation, measured with the circulation of the vortex, was achieved within t⁎= 1.5 compared to t⁎>4.0 in the absence of ground obstacle.

VIRTIS also revealed the intricacies of the inner region of the (southern) hemispheric vortex circulation (Garate-Lopez et al. 2015; Luz et al. 2011) which supplement the reflected light views that revealed the vortex from space time composites of Mariner 10 dayside images (Suomi and Limaye 1978) and Galileo (Peralta et al. 2007).

These waves can weaken the circulation around the polar vortex and make the polar vortex more susceptible to disruptions by northward-moving warm air masses and high pressure systems.

A striking example of this type of interaction is shown in sudden stratospheric warming events, which occur when the circulation of the polar vortex is disrupted, slowing down or even reversing the direction of the vortex winds during a period of a few days (Labitzke 1972 , 1981 Simmons 1974).