Dynamic turbulence

As dynamic turbulence in is meteorology the hydro- or aerodynamic induced turbulence of a flow designated due to wind shear in the atmosphere and friction at the surface. In meteorology, it is differentiated from thermal turbulence due to the warming of air layers with the resulting lift and convection.

Web links

• www.top-wetter.de

Individual evidence

1. ↑ For example Blüthgen, Weischet Allgemeine Klimageographie , de Gruyter 1980, p. 368, Gösta Liljequist, Konrad Cehak Allgemeine Meteorologie , Vieweg, 1994, p. 106