A Note on the bottom shear stress in oscillatory planetary boundary layer flow

Generally, there are some difficulties in application of the general similarity method to the problem of ideally dissociated air flow in the boundary layer around the porous

Numerical solutions of unsteady laminar boundary-layer flow caused by an impulsively stretching surface in the presence of a transverse magnetic field have been

GPU runtime and speedup as compared to one single- threaded CPU core for the first CUDA C version of the YSU PBL scheme after the L1 cache command cudaFuncCachePreferL1 is

However, for weak con- vective situations the lidar measurements reveal boundary layer heights that are higher compared to the microwave observations, because a decrease of the

Thus, in the lower third of the CBL the turbulent heat flux is posi- tively correlated with water vapour mixing ratio, i.e., the upward directed turbulent heat flux originated in

In Shortrun1 (Fig. 8c), the stratocumulus layer gets slightly thinner in general but the maximum in cloud water content increases and remains too far offshore, making the total

We achieve this for the special case of blood, but the underlying physical arguments may hold for any cell suspension constrained to the Newtonian regime of its rheology,

The method applied in this study to retrieve the entrainment zone thickness is likely suitable for situations with strong convection, so the data from lidar at SACOL on 14, 16, 22,