Investigating Buoyant Plume Dynamics Induced by Localized Fire-Simulated Heating over Plant Canopies Using LES

Abstract

The interaction of a buoyant plume with a plant canopy results in turbulent flow features distinct from those in a grassland environment. In this work, we model the turbulence dynamics of a buoyant plume in a homogeneous plant canopy with a crosswind using large-eddy simulations. As the plume interacts with the crosswind, we observe increased vorticity at the windward edge and tilted hair-pin-like vortical structures on the leeward side. Strong rotational cores, representing counter-rotating vortex pairs (CVPs), form as the flow twists and spirals into the leeward side of the buoyancy source from either side. Flow patterns aloft exhibit helical motions as the CVPs aloft propagate downstream, trailing the plume. We also simulate a no-canopy environment to facilitate comparison. The plume tilts less steeply near the source in the canopy case due to the canopy drag and its leeward side is marked by flow recirculation near the canopy top, which obstructs the upstream flow as it approaches. Moreover, the plume transition from the rise phase to the bent-over phase is delayed due to the canopy's aerodynamic effects and the oscillatory behavior of the far-field mean plume centerline is more damped. Additionally, in the canopy environment, there is downward momentum transfer primarily via ejections above the canopy and sweeps within the canopy space, upstream of the plume centerline. On the leeward side, counter-gradient motions play a significant role in transferring momentum away from the buoyancy source, with outward interactions being most dominant. Contrarily, in the no-canopy environment, counter-gradient motions near the surface are flanked upstream by an ejection-dominated region and downstream by a sweep-dominated region. Insights into the distinct plume behavior in canopy vs. no-canopy environments are vital for comparing with experiments and refining fire behavior or plume rise models.