92L still a threat to develop; record SSTs continue in the tropical Atlantic
A tropical disturbance (92L) over the Lesser Antilles Islands lost most of its heavy thunderstorms last night, due to an infusion of dry air. However, 92L has redeveloped a moderate amount of heavy thunderstorm activity this morning, and remains a threat to the Caribbean--though not as great a threat as it appeared yesterday. Satellite loops show that 92L's heavy thunderstorms are slowly growing in areal coverage, and are becoming more organized. St. Lucia reported sustained winds of 33 mph this morning in a heavy rain squall, and heavy rain showers and gusty winds can be expected throughout the southern Lesser Antilles Islands today. Martinique radar shows that heavy rains are now affecting that island, but there is no rotation to the radar echoes evident. Surface observations indicate that pressures continue to fall at a number of stations in the Lesser Antilles, but no surface circulation is evident in the wind reports. A strong flow of upper level easterly winds is creating a moderate 10 - 20 knots of wind shear on the south side of 92L. The waters are at near-record warmth, 30°C, and these warm waters extend to great depth. Water vapor satellite loops show a large area of dry air lies over the northern Caribbean, and this dry air could interfere with development over the next few days.
Forecast for 92L
The disturbance is moving westward at 5 mph, but steering currents favor a more west-northwest motion Saturday. Lower shear lies over the Central Caribbean, away from the coast of South America, so any northward component of motion will allow for more significant development. There is drier air to the north, but 92L is steadily moistening the atmosphere in the Caribbean, so dry air may not be a problem for it. Model support for development is less than it was yesterday. The GFS and NOGAPS models do not develop 92L. The HWRF, GFDL, and UKMET models predict development, with a track taking 92L into the Dominican Republic on Sunday as Tropical Storm Julia. These models predict the storm will continue west-northwest, affecting Haiti, Eastern Cuba, Jamaica, and the Southeast Bahamas early next week. The ECMWF model foresees a more southerly track, taking 92L into Mexico's Yucatan Peninsula seven days from now.
Residents of the northern Lesser Antilles Islands and Puerto Rico should anticipate the possibility of heavy rains from 92L affecting their islands on Saturday and Sunday, though most of the action will probably stay south and west. The southern Dominican Republic should see heavy rains of 3 - 6 inches on Sunday and Monday from 92L, and Haiti, Jamaica, and eastern Cuba should anticipate similar rains on Monday and Tuesday. Should 92L make a direct hit on the Dominican Republic, it could destroy the storm, though. NHC is giving 92L a 40% chance of developing into a tropical depression by Sunday, which is a reasonable forecast. The first Air Force Hurricane Hunter mission into 92L is scheduled for Saturday morning, but there will be two research missions into the storm today that will give us valuable information on 92L's large scale environment and potential for development.
Figure 1. Morning satellite image of 92L.
Igor
Tropical Depression Igor has survived a bout with high wind shear, and is now in an environment of moderate 10 - 20 knots of shear that should allow for steady strengthening. Waters are warm, 28°C, and the Saharan Air Layer (SAL) is probably not close enough to Igor to prevent development. The models continue to predict development of Igor into a hurricane 2 - 4 days from now. Igor will track west to west-northwest over the next week, with long range forecasts from the GFS and ECMWF models putting the storm several hundred miles northeast of the Lesser Antilles Islands about 6 - 8 days from now. Climatology shows that about 10% of all tropical cyclones that have existed at Igor's current position have gone on to hit the U.S. East Coast; these odds are about 5% for Canada. The forecast steering pattern for the coming two weeks from the GFS model shows a continuation of the pattern we've seen all hurricane season, with regular strong troughs of low pressure moving off the U.S. East Coast. This pattern favors Igor eventually recurving out to sea without affecting any land areas. The odds of Igor hitting land in the U.S. or Canada are probably close to their climatological 10% and 5% probabilities, respectively.
Elsewhere in the tropics
The GFS and ECMWF models predict the development of a new tropical wave off the coast of Africa 3 - 6 days from now.
August SSTs in the tropical Atlantic set a new record
Sea Surface Temperatures (SSTs) in the Atlantic's Main Development Region for hurricanes had their warmest August on record, according to an analysis I did of historical SST data from the UK Hadley Center. SST data goes back to 1850, though there is much missing data before 1910 and during WWI and WWII. SSTs in the Main Development Region (10°N to 20°N and 20°W to 80°W) were 1.23°C above average during August, beating the previous record of 1.01°C set in August 2005. August 2010 was the 7th straight record warm month in the tropical Atlantic. The five warmest months in history for the tropical Atlantic have all occurred this year; June 2005 comes in sixth place, and August 2010 in seventh. As I explained in detail in a post on record February SSTs in the Atlantic, the Arctic Oscillation (AO) and its close cousin, the North Atlantic Oscillation (NAO), are in large part to blame for the record SSTs, though global warming and Atlantic Multidecadal Oscillation (AMO) also play a role.
The Bermuda-Azores High was weaker than average during August, which drove slower than usual trade winds over the tropical Atlantic. These lower trade wind speeds stirred up less cold waters from the depths than usual, and caused less evaporational cooling than usual, allowing August SSTs to remain at record warm levels. The Bermuda-Azores High and its associated trade winds are forecast to be at near-average strength during the next two weeks, according to the latest run of the GFS model. This means that Atlantic SST anomalies will continue to stay at record warm levels during September, significantly increasing the odds of major hurricanes in the Atlantic.
Figure 2. The departure of sea surface temperature (SST) from average for September 9, 2010. Note the area of cool anomalies off the U.S. East Coast, due to the passage of Hurricane Earl. Cool anomalies are also evident east of Bermuda, due to the passage of Hurricane Danielle. Image credit: NOAA/NESDIS.
Next post
I'll have an update Saturday morning.
Jeff Masters
Reader Comments
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thanks for your synopsis and telling me what the CMC stood for earlier.
Quick question. As you noted in your synopsis from today that the next couple of systems exiting Africa will be coming off the coast further south than Igor and previous storms, are you saying that the it will be too far south to affected by the trough and go continuously west?
I guess it is too early to say obviously but if that is the case than the CONUS can breathe easy for now.
Agreed
Im trying, but my eye is not that good looking at this yet :(. I did see the cold fronts coming down the US that I imagine could pull Igor to the N.
Wait...so the trough is at 77W, and it's moving west, yet it's going to be at 63W by Saturday, then 67W by Sunday? I smell something, er, fishy... ;-)
You GOT to be kidding me! He just wont stay dead!
ATCF deactivated him 2 days ago.
Will they reactivate?
Why isnt this mentioned with a percentage on the NHC TWO, TWD, or graphic?
But now everyone that has him blocked has to see his post because you quoted him.
Since you didnt mention ex-Gaston, have you completed dismissed its possibility of regeneration? Thoughts?
Also, just for kicks, the trough that re curved both Danielle and Earl, was that trough stronger than the trough coming up at 55 to 60 W?
Just to compare because of the NHC saying that the ridge of high pressure building back after the trough passes and the fact that the models got it wrong on Earl.
Deep space probes aren't subject to the wind-and-wave action of a buoy, either. The fact that solutions exist for these problems does not necessarily mean that those solutions can be bundled into a rugged, low-power-consumption package that would survive contact with even a single cyclonic storm.
Hmm, that's about three fewer than it usually projects at any given time. I wonder why it's predicting such a dead period?
werent you screaming we wouldnt get but like 8 storms earlier ...
@everyone elese .. I know I know dont quote the trolls ...
Personally, I take stock and have more confidence in your forecasts! You're the man storm! thanks for your knowledge. you have taught me a lot.
I think I like yours better than mine!! LOL
LOL! :)
Storm-your opinion, do you see that trough h to lifting Igor up and out to sea or would Igor be far enough South to where that doesnt happen?
There are 2 systems here - dead Gaston & the broad area of low pressure, which is 92l. It is a bit confusing!
everyone keeps reading it wrong
this is explaining 2 separate systems folks. The first sentence is about Ex-Gaston which is at 77W and will be moving into Central America this weekend
The rest of it is about 92L
sorry to ask you this again but one thing I forgot to ask you is that when the NHC gave it's early morning advisory at 5, I think it spoke of some models building a ridge back in but the 11AM advisory then said "series of shortwave troughs affecting Igor turning him more WNW". This was not said at 5AM. does this mean that suddenly the series of shortwave troughs will keep the high from building back in? thanks
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