#3136 Postby NEXRAD » Tue Sep 02, 2008 3:51 pm
Aristotle,
Gustav's outflow is indeed circulating over Hanna, but the reason for that is an upper level ridge is present over the Eastern Gulf of Mexico. Therefore, Gustav is indirectly affecting Hanna, but a greater influence on Hanna is coming from the upper level flow that goes between the Gulf ridge and the trough off Nova Scotia. As the upper level air squeezes between these two features (offshore Georgia, roughly) the wind gets stronger and causes shear. As these winds approach Hanna, though, they spread out over a larger area, creating divergence. This divergence aloft helps to evacuate air from the convection around Hanna's center. This, likewise, helps the convection to keep going.
A good example of why the upper level winds help the system is noticed when comparing typical summer thunderstorms over the Southeast to those that occur with strong fronts. The basic explanation is as follows. The daytime thunderstorms occur in an environment with limited upper level wind. This causes the convection to build up and then collapse on itself, so the storms don't last that long. With strong frontal convection, the strong flow aloft helps the thunderstorm updrafts and helps keep the convection going.
- Jay
0 likes