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The boundary layer character is more pronounced in one direction as compared to the other.
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The boundary layer saturation is Eq. 18.
Boundary layer transition is caused by small disturbances within the boundary layer that grow via a variety of mechanisms to cause turbulence.
In contrast, above this boundary layer is the free troposphere; material entrained in this layer is typically subject to long-range transport.
The top of the daytime boundary layer is referred to as the mixed-layer inversion.
The fluid in the boundary layer is subjected to shearing forces.
The region above the planetary boundary layer is commonly known as the free atmosphere.
The boundary layer is turbulent, with a Reynolds number based on momentum thickness Req = 3200.
This boundary layer is approximately 0.3 nm thick.
A boundary layer flow was indirectly detected.
The boundary layer equations are (1).
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