Geodesic
On the three-dimensional laminar boundary layer with a rapidly oscillating external flow
Theoretical and applied mechanics, Tome 16 (1990) no. 1, p. 7 
R. Ašković; P. Florent; C. Tournier. On the three-dimensional laminar boundary layer with a rapidly oscillating external flow. Theoretical and applied mechanics, Tome 16 (1990) no. 1, p. 7 . http://geodesic.mathdoc.fr/item/TAM_1990_16_1_a1/
@article{TAM_1990_16_1_a1,
     author = {R. A\v{s}kovi\'c and P. Florent and C. Tournier},
     title = {On the three-dimensional laminar boundary layer with a rapidly oscillating external flow},
     journal = {Theoretical and applied mechanics},
     pages = {7 },
     year = {1990},
     volume = {16},
     number = {1},
     language = {en},
     url = {http://geodesic.mathdoc.fr/item/TAM_1990_16_1_a1/}
}
TY  - JOUR
AU  - R. Ašković
AU  - P. Florent
AU  - C. Tournier
TI  - On the three-dimensional laminar boundary layer with a rapidly oscillating external flow
JO  - Theoretical and applied mechanics
PY  - 1990
SP  - 7 
VL  - 16
IS  - 1
UR  - http://geodesic.mathdoc.fr/item/TAM_1990_16_1_a1/
LA  - en
ID  - TAM_1990_16_1_a1
ER  - 
%0 Journal Article
%A R. Ašković
%A P. Florent
%A C. Tournier
%T On the three-dimensional laminar boundary layer with a rapidly oscillating external flow
%J Theoretical and applied mechanics
%D 1990
%P 7 
%V 16
%N 1
%U http://geodesic.mathdoc.fr/item/TAM_1990_16_1_a1/
%G en
%F TAM_1990_16_1_a1

Voir la notice de l'article provenant de la source eLibrary of Mathematical Institute of the Serbian Academy of Sciences and Arts

In this article the three-dimensional laminar boundary layer with a rapidly oscillating external flow is discussed, because the problems in which the oscillations are superimposed on a stream are much more important in applications. Containing the supplementary components $Q_1$ and $Q_2$ of the pressure gradient, depending even of the normal coordinate n, the mean flow in our case differs considerably compared to the classical steady case. First, an approximate method to calculate both longitudinal and transverse velocity components of the mean flow is established. Then the method is applied to study the boundary layer (velocity, thickness, separation) on a sphere.