NW Carribean
Moderator: S2k Moderators
Forum rules
The posts in this forum are NOT official forecasts and should not be used as such. They are just the opinion of the poster and may or may not be backed by sound meteorological data. They are NOT endorsed by any professional institution or STORM2K. For official information, please refer to products from the National Hurricane Center and National Weather Service.
-
- S2K Supporter
- Posts: 6358
- Age: 62
- Joined: Sun Aug 31, 2003 1:01 pm
- Location: Miramar Bch. FL
- cycloneye
- Admin
- Posts: 146196
- Age: 69
- Joined: Thu Oct 10, 2002 10:54 am
- Location: San Juan, Puerto Rico
Dean4Storms wrote:This convective blow-up off the north coast of Honduras is looking suspicious too me. If it maintains overnight we may have a TD by tomorrow AM!!!
2 Things have to occur before we can say it will be a TD.First it has to persist for 24-36 hours meaning the convection and second it has to separate from land as right now land interaction is in place.
0 likes
Visit the Caribbean-Central America Weather Thread where you can find at first post web cams,radars
and observations from Caribbean basin members Click Here
and observations from Caribbean basin members Click Here
- SouthFloridawx
- S2K Supporter
- Posts: 8346
- Age: 46
- Joined: Tue Jul 26, 2005 1:16 am
- Location: Sarasota, FL
- Contact:
- mvtrucking
- S2K Supporter
- Posts: 698
- Age: 67
- Joined: Sat Jul 09, 2005 10:01 am
- Location: Monroe,La
-
- S2K Supporter
- Posts: 6358
- Age: 62
- Joined: Sun Aug 31, 2003 1:01 pm
- Location: Miramar Bch. FL
cycloneye wrote:Dean4Storms wrote:This convective blow-up off the north coast of Honduras is looking suspicious too me. If it maintains overnight we may have a TD by tomorrow AM!!!
2 Things have to occur before we can say it will be a TD.First it has to persist for 24-36 hours meaning the convection and second it has to separate from land as right now land interaction is in place.
Yea and no, we have seen TD's blow up alot faster than that with less deep convection and very close to land. Although what you state is a general rule, it is not without exceptions Luis.
Taking a look at IR imagery I see counterclockwise rotating convective cloud tops over the deepest convection and clockwise outflows at UL's especially on the north and eastern side of this deep convection. Like I said, if it maintians this overnite it could very well develop a closed low at the surface by 12:00 noon tomorrow, not saying it will, just that if it maintains this current deepening convection it could.
http://www.ssd.noaa.gov/goes/east/watl/loop-avn.html
0 likes
- Tampa Bay Hurricane
- Category 5
- Posts: 5597
- Age: 37
- Joined: Fri Jul 22, 2005 7:54 pm
- Location: St. Petersburg, FL
- SouthFloridawx
- S2K Supporter
- Posts: 8346
- Age: 46
- Joined: Tue Jul 26, 2005 1:16 am
- Location: Sarasota, FL
- Contact:
http://www.ssd.noaa.gov/goes/east/watl/loop-rgb.html
200mb analysis from the tafb indicates only 10kt shear over the gulf right now.
http://www.nhc.noaa.gov/tafb/QHQA17.jpg
I would watch to see if convection from the caribbean persists and a surface trough does develope in the southeastern gulf.
With Building High moving west from bermuda would create a more favorable environment and the trough scooting out to the northeast... stearing currents will be very weak.
If you look at the sat pics we may be seeing this starting to unfold.
http://www.ssd.noaa.gov/goes/east/watl/loop-rgb.html
Weak stearing currents will be left over in the gulf as the trough moves out.
http://cimss.ssec.wisc.edu/tropic/real- ... 8dlm2.html
200mb analysis from the tafb indicates only 10kt shear over the gulf right now.
http://www.nhc.noaa.gov/tafb/QHQA17.jpg
I would watch to see if convection from the caribbean persists and a surface trough does develope in the southeastern gulf.
With Building High moving west from bermuda would create a more favorable environment and the trough scooting out to the northeast... stearing currents will be very weak.
If you look at the sat pics we may be seeing this starting to unfold.
http://www.ssd.noaa.gov/goes/east/watl/loop-rgb.html
Weak stearing currents will be left over in the gulf as the trough moves out.
http://cimss.ssec.wisc.edu/tropic/real- ... 8dlm2.html
Last edited by SouthFloridawx on Thu Jul 06, 2006 9:16 pm, edited 1 time in total.
0 likes
-
- Category 1
- Posts: 264
- Age: 59
- Joined: Mon Jun 20, 2005 12:05 am
- Location: Ocean Springs, MS
Before a TD can form we need to have a low level circulation. This complex is a result of upper level diffluence southeast of an upper trough and surface convergence over the western Caribbean. As the strong/gale force trade winds over the central and western Caribbean reach central america there is convergence along the Honduras and Nicaragua coast. There is no low level circulation so therefore, no chance for a tropical cyclone to form in the near future.
0 likes
djones65 wrote:Before a TD can form we need to have a low level circulation. This complex is a result of upper level diffluence southeast of an upper trough and surface convergence over the western Caribbean. As the strong/gale force trade winds over the central and western Caribbean reach central america there is convergence along the Honduras and Nicaragua coast. There is no low level circulation so therefore, no chance for a tropical cyclone to form in the near future.
I agree...Maybe a weak MLC at 19.8/85.5 west with the tropical wave its self. But most of this is as you say air rising up/converging. Which can also be called a surface trough.
0 likes
- SouthFloridawx
- S2K Supporter
- Posts: 8346
- Age: 46
- Joined: Tue Jul 26, 2005 1:16 am
- Location: Sarasota, FL
- Contact:
Please of low level convergence over the se gom.
http://cimss.ssec.wisc.edu/tropic/real- ... 8conv.html
More than enough upper level divergence in the caribbean
http://cimss.ssec.wisc.edu/tropic/real- ... g8dvg.html
http://cimss.ssec.wisc.edu/tropic/real- ... 8conv.html
More than enough upper level divergence in the caribbean
http://cimss.ssec.wisc.edu/tropic/real- ... g8dvg.html
0 likes
-
- Category 5
- Posts: 4439
- Age: 31
- Joined: Fri Mar 10, 2006 7:36 pm
- Location: College Station, TX
http://www.ssd.noaa.gov/goes/east/watl/avn-l.jpg
What most tropical waves need for possible development is persistence..... and this system has persisted and stayed strong for a long time. I think that we might actually get a Tropical Cyclone from this system and we actually have something to watch.
What most tropical waves need for possible development is persistence..... and this system has persisted and stayed strong for a long time. I think that we might actually get a Tropical Cyclone from this system and we actually have something to watch.
0 likes
Personal Forecast Disclaimer:
The posts in this forum are NOT official forecast and should not be used as such. They are just the opinion of the poster and may or may not be backed by sound meteorological data. They are NOT endorsed by any professional institution or storm2k.org. For official information, please refer to the NHC and NWS products.
The posts in this forum are NOT official forecast and should not be used as such. They are just the opinion of the poster and may or may not be backed by sound meteorological data. They are NOT endorsed by any professional institution or storm2k.org. For official information, please refer to the NHC and NWS products.
- Tampa Bay Hurricane
- Category 5
- Posts: 5597
- Age: 37
- Joined: Fri Jul 22, 2005 7:54 pm
- Location: St. Petersburg, FL
Shear has lessened...oceanic heat content and SSTs are high, conditions
are becoming more favorable for development as explained by SouthFloridawx
in a post above.
Convection as of 10:40 PM EST looks intense over the Central America
Coastline and the NW Caribbean.
http://cimss.ssec.wisc.edu/tropic/real- ... xirg8n.GIF
are becoming more favorable for development as explained by SouthFloridawx
in a post above.
Convection as of 10:40 PM EST looks intense over the Central America
Coastline and the NW Caribbean.
http://cimss.ssec.wisc.edu/tropic/real- ... xirg8n.GIF
0 likes