The turbulent flow in and above plant canopies is of fundamental importance to the understanding of transport processes of momentum,heat and mass between plant canopies and atmosphere,and to microme- teorology.The Rey...The turbulent flow in and above plant canopies is of fundamental importance to the understanding of transport processes of momentum,heat and mass between plant canopies and atmosphere,and to microme- teorology.The Reynolds stress equation model(RSM)has been applied to calculate the turbulence in cano- pies in this paper.The calculated mean wind velocity profiles,Reynolds stress,turbulent kinetic energy and viscous dissipation rate in a corn canopy and a spruce forest are compared with field observed data and with Wilson's and Shaw's model.The velocity profiles and Rynolds stress calculated by both models are in good agreement,and the length scale of turbulence appears to be similar.展开更多
文摘The turbulent flow in and above plant canopies is of fundamental importance to the understanding of transport processes of momentum,heat and mass between plant canopies and atmosphere,and to microme- teorology.The Reynolds stress equation model(RSM)has been applied to calculate the turbulence in cano- pies in this paper.The calculated mean wind velocity profiles,Reynolds stress,turbulent kinetic energy and viscous dissipation rate in a corn canopy and a spruce forest are compared with field observed data and with Wilson's and Shaw's model.The velocity profiles and Rynolds stress calculated by both models are in good agreement,and the length scale of turbulence appears to be similar.
