TS Ernesto over the Caribbean Sea
Conditions around Ernesto have improved and now the storm is really starting to ramp up. The main issue was dry mid-level air and the storm’s fast forward motion. It simply could not line itself up vertically and allow for the convective process that drives its heat engine to work efficiently.
Water temps are plenty warm and it is obvious by looking at satellite imagery that the outflow is well established now. Ernesto should become a hurricane before the day is out.
The threat to the U.S. is all but gone now and so the focus will be on Central America, specifically Belize.
As it looks now, Ernesto will be intensifying as it makes landfall. This is never good news. As I have written about before, it has been our experience in dealing with hurricanes in the field that when they hit while intensifying, their effects are amplified. This is due to the convection or upward motion of the clouds that act to bring the strong winds down to the surface. We noticed this most notably during hurricane Charley in 2004 and never forgot what it was like. While Ernesto is not expected to become as strong as Charley, I hope that folks in Belize realize that this is not going to be a weak, sheared and dried out tropical storm when it hits- not anymore. Wind damage could be a real issue with Ernesto along with the other hazards of coastal storm surge and torrential rains.
Farther up the Yucatan where Cancun and Cozumel are, the impacts will be far less. Since Ernesto is not an especially large storm, its effects will be confined to the areas south of the northeast tip of the Yucatan. There may very well be some passing squalls from the outer rain bands but I do not see any reason to believe that Ernesto will post any big problems for Cancun and vicinity. In fact, that area is only under a tropical storm watch at this time. If you have plans to visit the area, do not cancel as Ernesto is only a problem farther south.
Once the soon-to-be hurricane crosses the Yucatan, it could get buried over Central America and rain itself out. This will obviously have negative impacts on the region with excessive rainfall a possibility. The official track does take the storm back out over the extreme southern Bay of Campeche with a final landfall in Mexico near the end of the week. How much time Ernesto spends over land will likely determine how strong it can get once it reaches the water again, if it does not simply die out over land.
The rest of the tropical Atlantic is quiet for now. Florence has dissipated and will likely not be able to make any appreciable comeback. We’ll see, you never know in August.
In the east Pacific, the NHC is keeping tabs on invest area 92E which is forecast to become a tropical depression and eventually a hurricane by many of the intensity models .However, the steering pattern continues to favor a general westward track away from Mexico. This is not typical of an El Nino year and lends more evidence to the fact that the atmosphere is not behaving as if we were in El Nino conditions. With a fairly strong high pressure area over the eastern Pacific it is no wonder that recent hurricanes in the east-Pac have moved westward. It is also keeping the progress of the developing El Nino at a slow pace which could have implications on the Atlantic season from here on out. I’ll discuss that in more detail in tomorrow’s blog post.