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Normal pollen counts occur immediately after the boundary layer.
As a result, this entrained air heats the boundary layer.
This region is called the "boundary layer".
Terrestrial radioactivity such as radon contributes additional ionization in the boundary layer over land masses72.
But as the flow rate decreases, the boundary layer re-attaches to the surface causing dribbling.
Above the boundary layer, but within the troposphere, the primary standard observation platform is the radiosonde.
The boundary layer is turbulent, with a Reynolds number based on momentum thickness Req = 3200.
Derivation of Navier-Stokes equations, the boundary layer approximations and boundary conditions.
The image to the right shows the trailing structure after upstream activation of the boundary layer.
Bernoulli's principle may be applied to when a fluid flows outside the boundary layer.
The fluid in the boundary layer is subjected to shearing forces.
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