Turbulence and Taylors
Hypothesis
- When studying turbulence (the spectrum of eddy sizes, for example), it is
difficult to obtain an instantaneous snapshot of the boundary layer and all
eddies formed within it.

- It is often easier and cheaper to make measurements of eddies in the
boundary layer at one point over a long period of time (i.e., a weather
station versus a Doppler radar)
- To study turbulence from a continuous record of measurements from a single
point, we need to assume that the
turbulence is frozen.
- What does this mean?
- As the mean flow advects the eddies past your sensor, the fundamental
properties of the eddies remain unchanged, or frozen. -->
- Mathematically, how can be express Taylors hypothesis?
For any variable, z, that can be used to study
turbulence, then the total derivative is equal to zero, i.e., dz/dt
= 0 if it is "frozen". We can write the total derivative as:
(1)
or
since dz/dt = 0 , (1) can be written as:
(2)
Considering
the example in the figure above, assuming that the flow is entirely in the x
direction, then then local change of the thermal's temperature will be given by:
(3)