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Chapter 6:
Atmospheric mixing
(PDF)
Previous chapters dealt solely with transport in various
water bodies and presented examples of onedimensional solutions to the transport equations.
We now turn our attention to transport and mixing in the atmosphere, and by necessity, we
will have to give more attention to threedimensional solutions.
Because of the atmosphere's unique composition and boundary and forcing conditions, atmospheric turbulence is more complicated
than the idealized homogeneous, stationary, isotropic case. Moreover,
these complications impact transport and mixing because they determine the values of the turbulent
diffusion and dispersion coefficients. Hence, a concise discussion of
atmospheric mixing requires studying atmospheric turbulence and the resulting modifications in the behaviour of mixing
coefficients from the idealized case.
This chapter begins with an introduction to atmospheric
turbulence and a review of turbulent boundary layer structure.
The logvelocity profile for a turbulent shear flow is introduced, and the behaviour of turbulence
throughout a neutrally stable atmospheric boundary layer is described.
Because of their importance to turbulence characteristics, the buoyancy
effects of heating and cooling within the boundary layer are discussed qualitatively.
The discussion on mixing begins with a review of turbulent mixing in
threedimensional, homogeneous, stationary turbulence. The solution for a continuous point source
is derived and used to illustrate mixing in the remaining section.
The chapter closes by adapting the idealized solution in homogeneous, stationary turbulence to the turbulence in
the atmosphere.
See Lecture
11.
