The method by which the meteorological data are
evaluated to determine the turbulent velocities, used in either
the puff or particle computation, is set in the Advanced / Configuration
Setup / Concentration menu (belowleft). Clicking on the Configure the
TURBULENCE method button produces the menu given belowright.



Turbulence Computation Methods
 Standard velocity deformation  The default method is defined by
a similarity approach for vertical mixing and velocity deformation for horizontal mixing.
K_{z} = k w_{h} z (1  z/Z_{i})
K_{h} = 2^{ 0.5}(c Δ)^{2}  ∂u/∂y + ∂v/∂x 
 Shortrange isotropic similarity  In shorter range dispersion simulations
(< 100 km) the deformation parameterization used in conjunction with larger scale meteorological
fields will not reflect the diurnal variations in horizontal turbulence. In this situation it is
desirable to use the short range parameterization in which the turbulent velocities
are computed directly from the stability functions instead of through the intermediate step
of computing a diffusion coefficient. The boundary layer velocity
variances are defined as a function of u*, w*, and Z_{i}.
This method does not use the diffusivity and no assumptions are required about
turbulent scales.
For instance, in the stable/neutral boundary layer:
w'^{2} = 3.0 u_{*}^{2} (1 – z/z_{i})^{3/2}
u'^{2} = 4.0 u_{*}^{2} (1 – z/z_{i})^{3/2}
v'^{2 } = 4.5 u_{*}^{2} (1 – z/z_{i})^{3/2}
 Input turbulent kinetic energy  If the turbulent kinetic energy (TKE) field is available from
the meteorological model, then the velocity variances can be computed from its definition
and the previous velocity variance equations to yield relationships with TKE.
E = 0.5 (u’^{2} + v’^{2} + w’^{2})
w’^{2} = 0.32 E, u’^{2} = 0.74 E, v’^{2} = 0.85 E
u’^{2 } = v’^{2} = 0.36 w_{*}^{2}
 Turblence velocity variance  Some meteorological data sets may already contain the component
turbulent velocity variances. This would normally be the case for
data that have been generated from local measurement programs.
The Puff growth computation method is used to define either the Linear or Square Root with time dispersion
equation for the horizontal growth rate of puffs. This option does not affect particle dispersion.
