Turbulence Intensity and
Turbulent Kinetic Energy (TKE)
- OK, thus far we have discussed how to separate the turbulent flow from the
large-scale, uniform flow
- The next question is:
- given a time series of wind speed observations, how can one
quantitatively determine the intensity of the turbulence?
- Recall that u' is the turbulent part of the flow and represents the
"deviation" of the total wind speed from the mean value:

- Q: What variable can we quantitatively compute that would represent
the intensity of turbulence? HINT: it
should have the same units as the variable being studied, so for wind speed,
this variable should have units of LT-1. Answer
- Yes, we need to use statistics to study turbulence!!!!!!
Variance (s2)
is one statistical measure of the dispersion of data about a mean value, and is
defined as:
(1)
where
N is the total number of points in your data set.
Recall that for flows where you can separate the mean value from the turbulent
part, you can write;
Ai
= A + a' (2)
where
Ai is the instantaneous value of that variable. Then you can
write (2) as
a'
= Ai - A
(3)
Substituting
(3) into (1) gives:
(4) or
(5)
Hence,
the average of the square of the turbulent part of a variable can be interpreted
as the variance of that variable.
The
standard deviation (s)
is related to the variance by
(6)
So,
as you can see from (6), if the standard deviation is large, then the turbulent
part of the flow is large, i.e., the turbulence
intensity is large.
A
dimensionless parameter that is often used as a measure of the turbulence
intensity (I) is given by:
I
= sU
/ M
(7)
where
M is the three-dimensional wind field.
Turbulent
Kinetic Energy
- One of the more important variables used to study turbulence and it's
evolution in the boundary layer is Turbulent
Kinetic Energy (TKE).
- If one again assumes that the flow can be partitioned into mean and
turbulent parts, then the total kinetic energy of the flow is simply the sum
of the kinetic energy of the mean and turbulent flows.
- Per unit mass, the kinetic energy of the mean and turbulent parts of the
flow can be expressed as:
(8)
where
MKE is the kinetic energy of the mean flow per unit mass, and e is
the kinetic energy of the turbulent flow per unit mass.
- The instantaneous values of TKE can vary dramatically, so it is often
useful to calculate a mean TKE value that is likely more representative of
the overall flow:
(9)
- TKE is generated by buoyant thermals and mechanically generated eddies
- TKE is suppressed or lost by layers of air that are becoming more stable
and is also dissipated into heat by the effects of molecular viscosity.
- Hence, one can write a TKE budget equation that is a sum of the production
and loss terms.
- if the production terms are larger than the loss
terms, TKE will increase and the boundary layer becomes more turbulent
- if the loss terms are larger than the
productions terms, TKE will decrease and the boundary layer becomes less
turbulent
- Later on in the course, we will write out the TKE budget equation and
physically interpret the various production and loss terms.
- In the mean time, a typical daytime diurnal variation of TKE for a
convective boundary layer is shown in Fig. 2.8

- The vertical distribution of TKE for three boundary layer types is shown
in Fig. 2.9. Do the vertical distributions make sense to you?

- Any questions???
- OK, let's do the TKE lab.