cycloneye wrote:Stephanie wrote:The majority of the models had Isabel pegged at hitting the EC in the MidAtlantic. The biggest problem was with the strength which FORTUNATELY was alot less than what she had originally grown to.
Yes Steph last year the forecast of the tracks was very good as I mentioned with Isabel and SF mentioned Claudette but still about forecasting intensity there is a ways to go and an example was Isabel at it's early formation how the forecast of the intensity was not so good that Isabel went from a wave to a hurricane in 2 days.
Good point that Luis brings up ... Intensity forecasts are simply the hardest to gauge and forecast ... there are so many small scale features that are happening continuously and various many factors that go into the process of trying to determine intensity forecasts, and they are FAR from perfect ...
Mesoscale features can cause a sudden burst of rapid intensification such as a warm water eddy, or a s/w ridge over the top of a TC (even for a brief period), or in Isabel's case, the appearance of Rossby Waves ... (or the swirls/mesovortices embedded within the larger scale eye.) ... and also, not to forget in stronger hurricanes, the eyewall replacement cycle, and this is only a few of the many factors that have to go into TC intensity forecasting ... let's not forget Hurricane Heat Potential (which in 98% of TC's are never realized) ...
Here's a PDF flie from AMS regarding estimations of Tropical Cyclone Strength...
http://ams.confex.com/ams/pdfpapers/72763.pdf
In Floyd's case, and also with Opal's case ... both passed over very warm eddies (In Floyd's case, I believe it was 32ºC water ... and in Opal's, well I can't quite remember, but I link this from the AOML page concerning this ...
Hurricane Opal in the Gulf of Mexico, August-September 1995 (left):
This TC intensified from hurricane-1 (74-95 mph winds) to hurricane 4 (131-155 mph winds) while traveling over a number of warm features in the Gulf of Mexico. In particular, this TC suddenly intensified from hurricane-2 (96-110 mph winds) to hurricane-4 in a period of 10 hours when its track went over a very well defined ring with a mean radius of 150 km that had been shed by the Loop Current. Altimeter-derived fields indicate that the increase in TCHP associated with this warm ring was approximately 30 kJ/cm2. The most striking information of the ocean conditions during the life span of this hurricane over the Gulf of Mexico was that this warm ring was not detected using the AVHRR-derived sea surface temperature fields.

Lili was a PRIME example of a rapid intensification stage, but quickly followed by an almost and just as rapid weakening phase just before landfall ... and just how hard it is to gauge when such cycles will occur ...
And unfortunately, I've lost my link to a page regarding Parameters for Rapid Intensification Paramaters ... I'll try to find those ...
SF