The foundation of statistical theory of turbulence will be examined and the problem of turbulent boundary layer flow over a flat plate in the presence of both heat and mass transfer will be described.

Geochemical observations appeared to support layering, whereas geophysical observations tended to support whole-mantle convection. The potential compositional boundary was typically put at 660 km ...

High-resolution model simulations are utilized to understand the connection between the micro-scale (cloud microphysics) and mesoscale motions, particularly in convective clouds. Several other key ...