Jeff Snyder
EF5
Just saw that update as well... Mind you, the 1730z report said central pressure was 923mb... So that's a fall of 9mb in 2 hours! This all while the hurricane is butting into some very dry air to its northwest...
Originally posted by David Wolfson
Next stop, Grand Cayman: http://www.caymanweather.metsite.com/WxFla...lash/redbay.htm
and http://www.weatherincayman.com/
Originally posted by rdewey+--><div class='quotetop'>QUOTE(rdewey)</div><!--QuoteBegin-David WolfsonNext stop, Grand Cayman: http://www.caymanweather.metsite.com/WxFla...lash/redbay.htm
and http://www.weatherincayman.com/
Thanks for the link! That data updates every few seconds! Should be real interesting to watch...[/b]
Originally posted by Chris Rozoff+--><div class='quotetop'>QUOTE(Chris Rozoff)</div>Originally posted by Jeff Snyder+--><div class='quotetop'>QUOTE(Jeff Snyder)I still can't believe it'd strengthen too much more.. I mean, there is some very dry air to the northwest of the system, which is likely some of the cause for the storm to become more asymmetric. .[/b]
Precipitable water from RAMSDIS experimental page doesn't really seem to bare this out. Yes, water vapor from GOES shows dry air, as it usually does in convectively inactive regions of the subtropics, but that, I believe, is somewhat misleading. The primary reason for the lack of signature in the water vapor to the storm's NW appears to be a disruption in the outflow of the hurricane. Nonetheless, the air is somewhat drier there aloft, no argument there. But I don't think this is unusual. The feature to its northwest and the building ridge to the storm's north, seems to be applying some shear on the storm. Shear will of course make the storm more susceptible to the dryer air aloft. Still, it is worth checking out the site:
http://www.cira.colostate.edu/ramm/rmsdsol/ROLEX.html
and glancing at the AMSU estimated precipitable water. This doesn't seem to suggest a terrifying environment of moisture for the storm to its NW. Actually, here's a downloaded picture: http://thunder.atmos.colostate.edu/~rozoff/29.gif
Best (and cheers to the renewed cat 5 status!),
Chris[/b]
Hmm... I started thinking about it again, and perhaps that 'dry' appearance is actually the descent of air around the edge of the hurricane (in combination with the shear that you suggested). All that rising air in the hurricane must sink somewhere (i.e. the eye and the area around the hurricane - near the ouflow). It will be real interesting though in the days to come with that trough/shortwave rotating southeastward across (over the central Plains right now), and it's effects on the hurricane.
Originally posted by Shane Adams
<!--QuoteBegin-rdewey@
<!--QuoteBegin-David Wolfson
Next stop, Grand Cayman: http://www.caymanweather.metsite.com/WxFla...lash/redbay.htm
and http://www.weatherincayman.com/
Thanks for the link! That data updates every few seconds! Should be real interesting to watch...
Originally posted by D. Bailey
Before I say anything else about what I've seen according to some of the models concerning Ivan, a bit of an update.
Ivan is back up to Category 5 intensity, the winds are 155 mph.
The Caymans ate getting hit and The Western portion of Jamaica is in the portion of Ivan that has storms close to the eye.
The 96-hour 500 mb heights+MSLP GFS Model shows Ivan very close to the AL/FL Border. It looks like this will be where the eye may very well make landfall.
There are a couple of Trofs (http://www.rap.ucar.edu/weather/progs/prog00hr.gif) that depending on speed, may affect movement of Ivan.
If the 96-hr 500 mb heights+MSLP GFS holds true, then target-wise the AL/FL border would be a good place for chasing.
Update on prressure in Ivan: As I was in the middle of working on this post, I heard on Tv in other room that the pressure is now 914 mb. Sorry, I don't know what network mentioned it.
MAX SUSTAINED WINDS 145 KT WITH GUSTS TO 175 KT.