Estimates vertical motions affecting heat and mass flux in the boundary layer, suggesting significant impact on weather patterns.
A method of estimating vertical motions that allows for diabatic heating was applied to the Daly Waters boundary layer experiment, in order to obtain estimates of heat and mass flux transfers across the top of the boundary layer.
No takes yet. Share an insight, caveat, or question.
I. D. Murphy (1979) studied this question.
Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context: