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The floor of the computational domain was populated with vertical fences in order to simulate a rough surface for boundary layer development, as in the experiments.
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Interactions between dry-air entrainment, surface evaporation and convective boundary-layer development.
Consequently, thickness of thermal boundary layer reduces as Pr increases.
The development of stimulate Tollmien-Schlichting waves in a boundary layer as a result of forced leading edge vibration is discussed.
A class of these solutions has proved to play an important role for describing the behavior of the fluid in the boundary layer and in the development of mathematical theories as well as in numerical computational schemes.
Up to a point, the boundary layer grows thicker as the lashes grow longer.
The top of the daytime boundary layer is referred to as the mixed-layer inversion.
The region above the planetary boundary layer is commonly known as the free atmosphere.
This suppression can limit the development of the boundary layer and results in a more stable boundary layer.
Boundary layers as rational approximations to the solutions of exact equations of fluid motion.
It is also shown that the fluid velocity field, as it changes with channel height, plays a small role in the development of the depletion boundary layer.
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