Boundary layer meteorology

fluid instability that occurs when there is velocity shear in a single continuous fluid or a velocity difference across the interface between two fluids

lowest part of the atmosphere directly influenced by contact with the planetary surface

layer in a fluid where there is a force balance between pressure gradient force, Coriolis force and turbulent drag

atmospheric measurement technique

physical constant in hydraulics

variable in atmospheric physics

dimensionless number

layer in which active turbulence has homogenized some range of depths.

wind model

layer of a turbulent fluid most affected by interaction with a solid surface or the surface separating a gas and a liquid where the characteristics of the turbulence depend on distance from the interface