weeniepatrol wrote:Thanks for showcasing this wave merging process!

I'm glad you liked it. It's not something that happens all too often, but it isn't uber-rare either. This probably wouldn't qualify as a true
binary (fujiwhara-type) interaction - while the lead wave slowed for the past couple of days, then basically stopped dead it its tracks as the merger took place, the effect on the track/speed of the trailing wave was negligible. The global model guidance 850 MB vorticity fields were unanimous that this would occur they just disagreed on when it would happen (check out some of my earlier posts that talk about the diffence between the ECM/GFS).
Speaking of which...
The axis of a strong tropical wave is near 56W, from 17N
southward, moving west at 20 kt. A recent scatterometer pass found
a distinct wind shift across the wave with fresh to strong winds
on either side north of 12N. Scattered weak convection is observed
from 10N to 16N between 49W and 59W.
2. Western Tropical Atlantic:
A tropical wave located a few hundred miles east of the Windward
Islands is producing disorganized showers and thunderstorms. Any
development of this system should be slow to occur while the wave
moves west-northwestward during the next day or two. The wave is
forecast to move over the Windward Islands today and then over the
eastern Caribbean Sea by the weekend, where further development is
unlikely due to unfavorable environmental conditions.
* Formation chance through 48 hours...low...10 percent.
* Formation chance through 5 days...low...10 percent.
Here's the ASCAT pass they mentioned. you can see a well-defined wind shift along the preimary wave axis, but you can also see that, as of the time of the pass, the waves hadn't quite merged 100 percent just yet. There were still two wave crests about 1.5 to 2 degrees apart.
