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9/30-10/5 Joaquin-Trough Interaction-DISCUSSION/OBS


bluewave

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 The equatorward outflow from Joaquin is amazingly good - its remarkably well-ventilated for such a sheared storm.  That (and the bathtub SSTs) is why the convection is so strong and persistent in the face of all the shear.  If the shear can simmer down this will strengthen fast - if poleward outflow can be established this will strengthen REALLY fast.

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Wow. That is pretty impressive then. Gotta think there will be changes tonight in the modeling as I don't think any models had this thing at 990 by this point.  Anyone know if the 18Z suite will have the recon data digested?

From pecking around other sites, I believe it will be the 0z suite that has the recon data. 

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 The equatorward outflow from Joaquin is amazingly good - its remarkably well-ventilated for such a sheared storm.  That (and the bathtub SSTs) is why the convection is so strong and persistent in the face of all the shear.  If the shear can simmer down this will strengthen fast - if poleward outflow can be established this will strengthen REALLY fast.

Establishing an anticyclone to the north would really help with that. Perhaps tomorrow?

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The cloud pattern of the storm has become better organized during

the day, with the low level center now embedded inside the northern

edge of the main area of deep convection. Animation of cirrus

motions suggest that upper-level outflow is becoming a little more

prominent over the northern portion of the circulation, and this is

consistent with decreasing northerly shear. Flight-level,

dropsonde, and SFMR wind observations from an Air Force

reconnaissance aircraft indicate that Joaquin has strengthened and

the intensity is now estimated to be 55 kt. With a more favorable

upper-level wind environment now expected to prevail, the official

forecast calls for more strengthening than the previous advisories.

Joaquin is expected to become a hurricane within 24 hours, with

additional intensification likely thereafter. The NHC intensity

forecast is similar to the latest SHIPS model output.

Fixes from the aircraft show a southward component of motion and

the initial motion estimate is now 240/4 kt. Joaquin is currently

south of the southwestern periphery of a weak mid-level ridge. The

ECMWF model shows this ridging to the north of the tropical cyclone

to be more prominent over the next few days than the other dynamical

models. Consequently, the ECMWF takes Joaquin more to the

west and southwest through 72 hours than any of the other available

guidance. Later in the forecast period, there is a significant

divergence in the track guidance. The HWRF and U.K. Met office

models forecast Joaquin to move over the East Coast of the United

States later in the period whereas the ECMWF and GFS keep the system

well offshore. The official forecast lies between these

possibilities and is similar to the latest Florida State University

superensemble solution.

Interests in the Bahamas should monitor the progress of this storm.

Watches or warnings may be issued for portions of these islands

later this evening.

Forecast positions and Max winds

Init 29/2100z 26.0n 71.0w 55 kt 65 mph

12h 30/0600z 25.8n 71.6w 60 kt 70 mph

24h 30/1800z 25.5n 72.5w 65 kt 75 mph

36h 01/0600z 25.1n 73.3w 70 kt 80 mph

48h 01/1800z 24.8n 73.9w 75 kt 85 mph

72h 02/1800z 25.0n 74.0w 80 kt 90 mph

96h 03/1800z 29.0n 73.0w 80 kt 90 mph

120h 04/1800z 34.0n 71.0w 75 kt 85 mph

$$

forecaster Pasch

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I thought this post from the main forum was to good not to pass on. I have to admit, it does sound awfully ominous

 

 

Once the low-level and mid-level centers become fully aligned, I truly believe that Joaquin will likely intensify faster than forecast. By days two and three, the storm will be wedged between a developing cutoff low over the Southeast and a cold mid-level trough over ex-Ida to its east. Such an environment is not only conditionally unstable, favoring rapid convective growth, but also, with a blocking high to the north, conducive to low ambient pressures as well as upper-level divergence.

This environment, filled with ample low-level moisture and high precipitable water, would support the development of dual outflow channels in the south and north quadrants of Joaquin, especially as the cutoff low becomes negatively tilted by day four and beyond. As Joaquin interacts with the trough, it may maintain its intensity or deepen even further on day four, thanks to some indirect baroclinic influences, as the storm initially parallels the mean shear vector.

Already, Joaquin is clearly organizing even though the centers are not yet fully aligned. The storm is clearly intensifying faster than originally expected, and even the deterministic ECMWF is likely underestimating the rate of deepening, showing 990 mb by 12Z tomorrow, even though the pressure is already down to that level. An excellent outflow channel is already established in the southern quadrant, and the nascent CDO is slowly expanding westward as northerly shear lessens.

Based on all indications, significant, quite possibly rapid intensification will commence tomorrow, as an upper-level anticyclone builds over the system. Thus, Joaquin will likely have about four full days (Wednesday through Saturday) to intensify significantly. The stronger intensity in the short term would likely bring the cyclone into the east-central Bahamas in little more than two days, with the deeper system enhancing mid-level heights to its north. The ECMWF ensembles have consistently shown this.

Given all indications and trends, I would not be surprised if Joaquin becomes a significant hurricane (85+ kt) as it meanders over the east-central Bahamas on Thursday and Friday. A potentially severe impact to the Bahamas (Eleuthera, Cat Island, San Salvador, and possibly even the Exumas) is becoming more plausible. The 1929 Bahamas hurricane underwent rapid deepening in a similar set-up; Joaquin may well follow its example, only farther east.

 

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