Book of Donmon Teith

Vertical transport in the stratosphere occurs by many processes and the question of the relative importance of stratified turbulence is considered in the contex

The determination of winds and temperature by rawinsonde allows us to calculate the Richardson number, a measure of atmospheric instability. From this, we can t

This paper reviews the estimates to date of the vertical 'effective diffusion coefficient' for stratospheric small scale turbulence transport, KB. These estimat