ncweatherwizard wrote:Eh...it's not really ventilation of the outflow that causes the strengthening, but you've basically got the right idea. QG dynamics will tell you that divergence occurs in the upper troposphere ahead of an upper level trough because the winds in a trough are subgeostrophic (and the winds in the downstream ridge are supergeostrophic). So the winds exiting the trough are faster, and you horizontally advect more mass out of a region ahead of a trough than you advect in. Coincidentally, this is also the area where you often see strong SW winds aloft, which causes the cirrus outflow to expand over a large area. But it is really the large-scale divergence and vertical motion in the upper-troposphere that allows the strengthening. This process is baroclinic enhancement of a tropical cyclone.
Thanks for the explanation.