layers, show a substantial increase of intermittency in comparison with isotropic conditions.
This suggests a close link between anisotropy and intermittency. However, a rigorous
statistical description of anisotropic flows is, in most cases, hampered by the inhomogeneity
of the field. This difficulty is absent for homogeneous shear flow. For this flow the scale-by-
scale budget is discussed here by using the appropriate form of the Kámán–Howarth …