robjay wrote:http://orca.rsmas.miami.edu/wximages/jet/1_05/anis.html
If you give the above link a look, you can see what appears to be UL winds steering storms in a clockwise motion, yet tropical storm events are counter clockwise. I'm trying to understand what would identify an ideal area of possible development in the above water vapor imagery? Are the "steering clockwise wind currents" a shear type force on tropical development?
Thanks -
You're mixing up a number of things here.
First of all: steering flow. What layers affect the movement of a storm depends on how strong the storm is (you'll sometimes see this referred to as how "deep" it is). Weaker systems tend to be steered by the lower layers, stronger systems by more and more of the column. Upper level winds have the least effect on steering.
However, upper level wind do play a big part in how much convection a system has and how that convection is situated with respect to the low-level circulation (LLC). The ideal setup for a storm is to have an upper level high above it with flow away from that high on all sides.
A sheared situation, as we see with 94L in the Bahamas, for instance, causes the convection to be located on the downwind side (in 94L's case northeast of the disturbance's center) which inhibits development as low-level convergence does not correspond with the circulation center.
Hope that helps.
Jan