

http://www.met.nps.edu/~mtmontgo/storms2012/P09L.html
SYNOPSIS 2012072800
* Still working on GFS computer issues.
P09L
10N, 4W
700 hPa
ECMWF: Phase speed is based upon v700 during days 3-5. Uncertain positions as I track a tiny OW max within the monsoon trough over West Africa for the first 48 hours. As soon as it moves over the ocean, though, a distinct pouch is depicted fairly quickly that continues to move westward.
GFS:
UKMET: Several uncertain positions when depicted as only an OW max. When it moves out over the Atlantic, P09L is simply a zonally-elongated ITCZ circulation that doesn't move westward, at least not quickly. I stop tracking at that point at 72 hours.
NOGAPS: NOGAPS does actually have an OW max in the same area, and it moves westward out over the ocean, where it stalls. Eventually, a pouch with a CL-trough intersection is also depicted there at day 4 that starts to move slowly westward. So, although slower than ECMWF, NOGAPS has about the same story. However, I don't track anything because four days is too long for me to assign uncertain positions based only upon an OW max. Note that I had to use the v850 Hovmoller to find some sort of signal.