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Atlantic Tropical Action 2014


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WEATHER RECONNAISSANCE FLIGHTS
CARCAH, NATIONAL HURRICANE CENTER, MIAMI, FL.
0530 PM EDT WED 10 SEPTEMBER 2014
SUBJECT: TROPICAL CYCLONE PLAN OF THE DAY (TCPOD)
VALID 11/1100Z TO 12/1100Z SEPTEMBER 2014
TCPOD NUMBER.....14-102 AMENDMENT

I. ATLANTIC REQUIREMENTS...ADDED
1. SUSPECT AREA (NEAR BAHAMAS)
FLIGHT ONE -- TEAL 71
A. 11/1730Z
B. AFXXX 01HHA INVEST
C. 11/1445Z
D. 27.0N 77.5W
E. 11/1700Z TO 11/2200Z
F. SFC TO 10,000FT

FLIGHT TWO - TEAL 72
A. 12/0530Z, 1130Z
B. AFXXX 0206A CYCLONE
C. 12/0215Z
D. 27.0N 78.5W
E. 12/0500Z TO 12/1130Z
F. SFC TO 10,000FT

2. OUTLOOK FOR SUCCEEDING DAY.....CONTINUE 6-HRLY
FIXES IF SYSTEM DEVELOPS AND REMAINS OFFSHORE.
3. REMARKS: NASA 872 RESEARCH FLIGHT AT 12/2200Z.

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The upper level winds on the backside of the huge upper level ridge over the SE US is going to put some marginal to strong (20-30kts) over 92L in about 24 hrs. It has until then to get it's act together. Maybe if it gets going quick it can make it to TD/Low-end TS but after that window is closed, it's development is going to be stunted.

That's right...although a deeper system would feel a little less shear, as it would probably be moving faster in the mid/upper level steering currents...anyway, like you said it has 24-48 hrs to organize in a relatively low shear environment.

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That's right...although a deeper system would feel a little less shear, as it would probably be moving faster in the mid/upper level steering currents...anyway, like you said it has 24-48 hrs to organize in a relatively low shear environment.

 

 Looking at infrared satellite photos this evening, I see renewed healthy convection as older dies out. I'm now thinking 2/3 chance of a TD+ while still E of FL due to current conditions being so favorable (well organized with small size/good moisture/high SST's/upper high/light shear/far enough from land since Bahamas don't interfere much).  Anyone disagree?

 

 Edit: Another way to put this: how much more favorable a combo of factors can there be? Are the overall factors as favorable as they seem to me?

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 Looking at infrared satellite photos this evening, I see renewed healthy convection as older dies out. I'm now thinking 2/3 chance of a TD+ while still E of FL due to current conditions being so favorable (well organized with small size/good moisture/high SST's/upper high/light shear/far enough from land since Bahamas don't interfere much).  Anyone disagree?

 

 Edit: Another way to put this: how much more favorable a combo of factors can there be? Are the overall factors as favorable as they seem to me?

 

I agree that the environment 92L is presently in is quite good.  However, shear has been increasing steadily just 100-200 km to its north, and there's also some subsidence in the area.  The fact that it's such a small system will make it more vulnerable to a deterioration of its environment.  I'd say it's best chance is if it begins drifting southward overnight.  A track along the lines of the NAM would probably be ideal. 

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92L is certainly intriguing. The circulation still appears to be closed, with a decent amount of westerly winds to the south of the convection over the Bahamas. Note the interesting wind shift that took place in Great Abaco Bahama earlier today. While 10-15 knot westerlies might not sound like much, that's more than what the global models are depicting currently. The easterly winds are likely stronger in the northern quadrant where the deep convection is ongoing. Pressure is still steady around 1014 hPa, but should typically be rising in a typical diurnal cycle. It will be interesting to watch these stations to see if there are any significant changes during the overnight hours. 

 

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There is a really strong shear axis just to its north which is dropping south with time. So I agree 92L will probably have to keep dropping south if it wants to survive. However, I don't think the global models have an adequate depiction of the current organization of the circulation. Small systems like this often fly under the radar so to speak, and sometimes these relatively small llc's that form from upper-level TUTTs can be suprise developers (e.g. Michael 2012).

 

The key though is the convective organization. If it can build a symmetrical cirrus canopy, small systems like this can spin up quickly. If it doesn't do that before the shear hits though, its game over.  

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As the mid/upper ridge strengthened, so the shear has increased as well. Now we have a decoupled mid and low level vortices. The surface low is still north of the Abaco Islands, while the mid level vortex is moving WSW and is currently north of the Grand Bahama...unless there's a better stacked up low, I expect little development in the short term.

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As the mid/upper ridge strengthened, so the shear has increased as well. Now we have a decoupled mid and low level vortices. The surface low is still north of the Abaco Islands, while the mid level vortex is moving WSW and is currently north of the Grand Bahama...unless there's a better stacked up low, I expect little development in the short term.

Would a stronger ridge to the north lend more confidence in a southern FL track rather than Central FL?

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As the mid/upper ridge strengthened, so the shear has increased as well. Now we have a decoupled mid and low level vortices. The surface low is still north of the Abaco Islands, while the mid level vortex is moving WSW and is currently north of the Grand Bahama...unless there's a better stacked up low, I expect little development in the short term.

Now that I take a closer look at the radar, I do see two distinct circulations with the mid level one being more SW. It's probably compliments of shear since the main convection is moving SW along with the shear.
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I agree that the environment 92L is presently in is quite good. However, shear has been increasing steadily just 100-200 km to its north, and there's also some subsidence in the area. The fact that it's such a small system will make it more vulnerable to a deterioration of its environment. I'd say it's best chance is if it begins drifting southward overnight. A track along the lines of the NAM would probably be ideal.

It looks like the quite good conditions for development that we agreed were there yesterday have deteriorated due to the NE shear that you noted increasing just north of the system last night. It doesn't look as stacked to me now and it didn't take long for this to occur as it was still looking pretty good well into the evening. My prior thinking of 2/3 chance for TD+

while still E of FL is looking quite a bit too high to me now despite there apparently still being a pretty good LLC.

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Even though the vertical wind shear is increasing over 92L, note that the the upper-levels will also be very diffluent over 92L as the upper-level low to 92L's northeast is causing some upper-level wind vectors to shift back westerly. This is one of the reasons the initial dry air over the region has moistened rapidly the last 12-18 hours. This should also allow convection to continue to pulse which will mitigate the strongest easterly vertical shear the next 24-48 hours. Center relocations south and west further into the deep convection are also entirely possible, and in fact might be trying to occur currently. 

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