Tropical Depression Six arrives
Tropical Storm Tropical Depression Six is here, but it will not be a threat to land for at least the next five days. Tropical Depression Six is a classic "Cape Verdes"-type storm common during the peak part of hurricane season. Cape Verdes-type storms are so named because they form from tropical waves that come off the coast of Africa and pass near the Cape Verdes Islands just west of Africa. Cape Verdes hurricanes are the largest and most dangerous types of hurricane in the Atlantic, since they spend a long time over water have and have of opportunity to reach full maturity. Tropical Depression Six has a ways to go before it becomes a hurricane, as the storm is embedded in a strong easterly flow of wind courtesy of the African Monsoon that is generating a moderately high 15 - 20 knots of wind shear. There is also a tropical disturbance to the northeast of TD 6 that is sucking away some moisture and is interfering with the storm's circulation. Sea Surface Temperatures (SSTs) are a warm 28°C, and the storm is embedded in a moist environment, so wind shear is the primary inhibiting factor for development. The strong east winds imparting the shear are keeping any heavy thunderstorms from developing on the east side of the center of circulation, which is exposed to view in satellite imagery (Figure 1.)

Figure 1. Afternoon satellite image of Tropical Depression Six.
Forecast for Tropical Depression Six
A ridge of high pressure will force Tropical Depression Six to the west-northwest for the next five days, and the system should increase its forward speed from its current 10 mph to 15 mph by Monday night. A powerful trough of low pressure over the mid-Atlantic Ocean will begin to pull Tropical Depression Six more to the northwest late this week, and the storm should pass well to the northeast of the Lesser Antilles Islands. It remains to be seen, however, it this trough will be strong enough to fully recurve Tropical Depression Six out to sea. The GFS predicts that Tropical Depression Six may pass close to Bermuda about eight days from now, and it is also possible that Tropical Depression Six could eventually hit the U.S. East Coast 9 - 15 days from now. However, we have no skill in making these sort of ultra-long range forecasts, and the long-range fate of TD 6 is uncertain.
Elsewhere in the tropics
The ECMWF and NOGAPS models are predicting formation of a tropical depression off the coast of Africa 3 - 4 days from now.
Jeff Masters
Reader Comments
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The circulation is on the eastern edge of the convection. Its been said many times.
- Date - - - Time - - - - - Location - - Windspeed - Pressure
22Aug - 06amGMT - 11.7n33.0w - - 30knots . . . . 1007mb - NHC-ATCF *was11.8n*
22Aug - 09amGMT - 12.1n33.4w - - 35mph . . . . . 1007mb - NHC.Adv.3
22Aug - 12pmGMT - 12.2n33.9w - - 30knots . . . . 1007mb - NHC-ATCF
22Aug - 03pmGMT - 12.7n34.1w - - 35mph . . . . . 1007mb - NHC.Adv.4
22Aug - 06pmGMT - 13.2n34.6w - - 30knots . . . . 1007mb - NHC-ATCF
*before NHC reevaluated&altered TD6's path*
22Aug - 09pmGMT - 13.4n35.1w - - 40mph . . . . . 1005mb - NHC.Adv.5
23Aug - 12amGMT - 14.0n35.3w - - 40knots . . . . 1003mb - NHC-ATCF
23Aug - 03amGMT - 14.2n35.9w - - 50mph . . . . . 1000mb - NHC.Adv.6
23Aug - 06amGMT - 14.8n36.0w - - 45knots . . . . 1000mb - NHC-ATCF
40knots=~46mph _ _ _ ~43.5knots=50mph _ _ _ 45knots=~51.8mph
NHC rounds windspeeds to the nearest 5mph or to the nearest 5knots
Copy&paste 13.2n34.6w-13.4n35.1w, 13.4n35.1w-14.0n35.3w, 14.0n35.3w-14.2n35.9w, 14.2n35.9w-14.8n36.0w, hex, bda, sid into the GreatCircleMapper for a look at the last 12hours.
I highly doubt that the circulation is directly under the deep convection. Its more than likely stuck in the right quadrant due to the 20 knots of easterly shear.
As Korithe was saying, if the center was in the deep convection we'd be seeing more outflow on the eastern side.
Ah, okay. Sorry for the misunderstanding.
the heaviest convection is wrapped around it, and the CDO like feature that it has developed is spinning around that area the strongest, so either it has a MONSTER MID LEVEL LOW or that's where the center is.
Because even though there is easterly shear, it's still breathing on the east side.. showing how strong the thing is becoming how it's literally fighting the shear
Tropical Cyclone Advisory #9
TROPICAL STORM MINDULLE (T1005)
15:00 PM JST August 23 2010
===============================
SUBJECT: Category One Typhoon In South China Sea
At 6:00 AM UTC, Tropical Storm Mindulle (994 hPa) located at 16.2N 109.9E has 10 minute sustained winds of 35 knots with gusts of 50 knots. The storm is reported as moving west northwest at 11 knots
Dvorak Intensity: T2.5
Gale Force Winds
=================
150 NM from the center
Forecast and Intensity
=======================
24 HRS: 18.2N 106.5E - 45 knots (CAT 1/Tropical Storm)
48 HRS: 19.5N 104.1E - 40 knots (CAT 1/Tropical Storm)
72 HRS: 20.5N 102.0E - 30 knots (Tropical Depression)
Your fix puts the center in the center of the convective burst. I am fixing the center between where you are and ADT is, like at 14.5 N 36.3 W.
Keep her away from CONUS
I don't think its under the deepest convection, but I don't think its as far east as ADT puts it either (see post 2712). I think its under the northeast side of the convective blob, not right at the edge of the convective blob like ADT has it.
Anyways, this wave will likely be our next invest.
I'm not just looking at the fact that's the strongest convection, I'm looking at the possibility that, that is where the strongest spin is located on infared
http://www.ssd.noaa.gov/goes/flt/t1/loop-ft.html
if you look at the northern side of the convection you can see the spin clearly, that's what I see, could it be wrong? Sure, but if it is then it's one very disorganized system, and there is no way that it is stacked, if it's stacked that's where the center should be imo
Your estimate seems pretty plausible.
I hate to tell you this, its probably tilted westward with height so any spin well-embedded in the deep-convectin is possibly a mid-level spin west of the surface spin.
I do agree with you that she's fightin' the shear, and fightin' hard like a true champion. Even if its not perfectly vertically stacked, a system fighting this hard in shear can gradually strengthen in the shear.
This shortwave infrared loop may help you in seeing the low-level spin easier.
http://www.ssd.noaa.gov/goes/flt/t1/flash-ir2.html
Ignore the blue-colored clouds, those are the high cloud tops that distract you from seeing where the low-level center is. The black clouds are the low-level clouds, and looking carefully during the animation, you can see a swirl moving west and west-northwest into the east edge of the blue clouds. That swirl is the surface center of Danielle.
I would suggest checking the sheer maps, those aren't cirrus, but are feathering of the upper levels of the CDO. I believe that would mean that the anticyclone much talked about in previous hours is approaching alignment with the CDO, as this is evidence of outflow sheer.
Atmo or StormW, I believe that's your expertises though. Just my obs.
Feathery clouds at the top of a CDO is technically called cirrus clouds. The anticyclonic center of cirrus outflow is currently west of the low-level center right now because of the easterly shear.
That tropical wave, yep it looks good. Just entertaining thought here, maybe this could eventually become major hurricane earl eventually, that would be neat. As far as I remmeber, there has never been a major hurricane earl (cat. 3 or higher) before. The strongest earl I know was cat. 2 earl in 1998.
Earl is such a funny name for a powerful storm IMO.
Jason, ROFL, LOL. That music on that video sure beats the local on the 8s music on the weather channel. I think Danielle likes that rock music. Careful, play it too long, and she might strengthen too much, LOL!
:0
update
Almost due West.......which the Steering graphics show it should be almost due West.
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