Buoy 42056 located at 19.9N, 85.0 W recently had the winds shift from the south to the west and increase to 23 knots sustained. This either indicates that there is a surface low located somewhere to its north near the Yucutan channel, or that the deep convection in that area is in the form of a squall line that is producing some gusty outflow winds along its leading flank. Considering the increase in wind speed, the rise in pressure, and the apparent circulation over the Yucutan is still well to the west, the squall line scenario seems more likely. If that is the case, it would not be surprising to see that area of convection weaken or even puff out at some point. Whether or not the circulation still over the Yucutan can redevelop convection and wrap it around the center will determine if this thing develops or not.
0 registered and 243 anonymous users are browsing this forum.
Moderator:
Forum Permissions
You cannot start new topics
You cannot reply to topics
HTML is disabled
UBBCode is enabled
Rating:
Thread views: 46172
Note: This is NOT an official page. It is run by weather hobbyists and should not be used as a replacement for official sources.
CFHC's main servers are currently located at Hostdime.com in Orlando, FL.
Image Server Network thanks to Mike Potts and Amazon Web Services. If you have static file hosting space that allows dns aliasing contact us to help out! Some Maps Provided by:
Great thanks to all who donated and everyone who uses the site as well.
Site designed for 800x600+ resolution
When in doubt, take the word of the National Hurricane Center