BUOYANT FLOW CHARACTERISTICS WITH THERMAL CYLINDERS IN STABLY STRATIFIED AIR

ABSTRACT A flow induced by thermal cylinders at neutral (st = 0) or stable (0 < st) stratification, where st is the stratification degree, is analyzed numerically. As a result, a new kind of flow resulting from thermal cylinders is discovered, and agrees well with the previous experimental result of flow visualization as follows: At 0 ≤ st, the thermal cylinder flow (TCF) is defined as the flow due to a thermal cylinder, and is generated intermittently. A TCF rises and develops to a small roof-shape flow, which separates to the right and left directions near the thermal flow front. Then, at st = 0 and a small st, one edge of a layer is fixed near the midplane, and another edge of a layer moves outward. Thus a nonslip-type layer is formed. Furthermore, because many thermal cylinders arrive intermittently at the front, many layers of nonslip type are formed. On the other hand, at a large st, all the layers slip off the midplane, and move slowly outward. As a result, many layers of slip type are formed.

[1]  Ephraim M Sparrow,et al.  Observations and other characteristics of thermals , 1970, Journal of Fluid Mechanics.

[2]  J. Giovannoni A laboratory analysis of free convection enhanced by a heat island in a calm and stratified environment , 1987 .

[3]  T. Nakajima,et al.  Spectra and critical Grashof numbers for turbulent transition in a thermal plume , 1999 .

[4]  K. Noto,et al.  Swaying motion in thermal plume above a horizontal line heat source , 1989 .

[5]  Katsuhisa Noto,et al.  TEMPERATURE FIELD WITH THERMAL CYLINDERS IN BUOYANT FLOW IN STABLY STRATIFIED AIR , 2005 .

[6]  William H. Snyder,et al.  A Laboratory Study of the Urban Heat Island in a Calm and Stably Stratified Environment. Part II: Velocity Field , 1997 .

[7]  Thermal Plume Turbulent Enhancement, Reverse Transition, and Relaminarization in Stably Stratified Enclosure , 2001 .

[8]  G. Desrayaud,et al.  Modeling a horizontal heat-flux cylinder as a line source , 1994 .

[9]  K. Noto Dependence of heat island phenomena on stable stratification and heat quantity in a calm environment , 1996 .

[10]  Guy Lauriat,et al.  Unsteady confined buoyant plumes , 1993, Journal of Fluid Mechanics.

[11]  Kenneth E. Torrance,et al.  Natural convection in thermally stratified enclosures with localized heating from below , 1979, Journal of Fluid Mechanics.

[12]  GENERATION OF THE KARMAN VORTEX STREET AT LOW REYNOLDS NUMBER DUE TO COOLING A CYLINDER: CAUSE AND FLUID TYPE EFFECT BY NUMERICAL COMPUTATION , 2001 .