ATL: JOAQUIN - Models
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- TheProfessor
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I'm still learning to read maps, but is there a weakness near ex-Ida yet? because if it isn't there yet it seems like that would keep the storm further west until it possibly develops.
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spiral wrote:The EC has to verify until then its to early to be singing praise's :
Well compared to the GFS handling Joaquin since it formed, the Euro is winning so far. And I go with the model that has been the most persistent and consistent, the Euro.
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i,agree. It's ridiculous. The facts are that the gfs and euro are 50 50 from 2012 - 2014. Further, the storm isnt over so there is no verfication. I really wish something would be done with the non sense. If the euro is right then good it needed a huge win this year. It's not like cheering for a super bowl team. The more accurate all of the models are, the better for everyone. Lives saved, property saved, money saved form needless evacuations, preparations, etc... It's misleading for the newbies that come on here for this hyberbole.I've never understood the modeling wars.Alyono wrote:lets not forget the FIRST model to show an east coast landfall with Joaquin was THE EURO
The hugging of this model is borderline cultish in that everyone ignores the failures
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Re: ATL: JOAQUIN - Models
Models are not a sport, and I honestly do not care what individuals think of the models. In my role as moderator I don't think these kinds of discussion add any value to this thread so I'm asking people to stop. Thanks. 

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M a r k
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Re:
Stormcenter wrote:Correct me if I'm wrong but wasn't the EURO the only model last week to show two weak two lows in the GOM earlier this week? One in the western and the other in eastern GOM. I believe that is exactly how it played, just saying.
You are correct, it did well with 99L but at the same time it did not do that well with Ida.
Regarding Joaquin, I have always said that if it hangs around longer around the central Bahamas the less threat it will be for the mid Atlantic States, on the last few runs the GFS started following the Euro in keeping Joaquin down there longer thus it started trending to the right.
But Joaquin could still be a threat to New England if ridging in the NW Atlantic stays put, time will tell.
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Re: ATL: JOAQUIN - Models
these models are like baseball players, they go 0-3 sometimes and they can go 4-4 but the difference is GFS is the sammy sosa of baseball the euro is the Barry Bonds of baseball 

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- Yellow Evan
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Re: ATL: JOAQUIN - Models
Code: Select all
* ATLANTIC SHIPS INTENSITY FORECAST *
* IR SAT DATA AVAILABLE, OHC AVAILABLE *
* JOAQUIN AL112015 10/01/15 12 UTC *
TIME (HR) 0 6 12 18 24 36 48 60 72 84 96 108 120
V (KT) NO LAND 110 111 111 112 112 115 113 104 96 82 71 62 51
V (KT) LAND 110 111 111 112 112 115 113 104 96 82 71 62 51
V (KT) LGE mod 110 111 110 109 109 109 111 104 89 72 59 50 43
Storm Type TROP TROP TROP TROP TROP TROP TROP TROP TROP TROP TROP TROP EXTP
SHEAR (KT) 15 12 9 4 5 8 16 21 28 32 34 36 36
SHEAR ADJ (KT) 11 16 17 14 10 4 5 7 7 6 0 7 9
SHEAR DIR 3 16 14 10 320 288 303 274 264 237 219 222 240
SST (C) 29.7 29.7 29.7 29.8 29.8 29.8 29.5 28.2 27.8 26.8 26.5 25.1 22.4
POT. INT. (KT) 161 161 161 164 165 166 161 141 135 120 116 106 90
ADJ. POT. INT. 140 139 140 147 147 149 145 126 116 98 95 91 80
200 MB T (C) -51.6 -51.0 -51.0 -51.0 -50.9 -50.1 -49.7 -48.5 -48.5 -48.7 -49.2 -49.4 -49.6
TH_E DEV (C) 10 11 11 10 10 9 8 8 4 1 0 0 0
700-500 MB RH 61 64 65 66 66 63 54 46 57 62 62 61 46
MODEL VTX (KT) 30 32 34 34 33 38 40 39 40 38 39 41 40
850 MB ENV VOR 68 83 89 102 123 147 183 240 166 124 138 129 133
200 MB DIV 46 42 26 51 75 72 94 49 73 59 74 56 14
700-850 TADV 6 11 12 7 11 17 22 68 80 68 58 8 -25
LAND (KM) 300 266 233 271 321 522 635 540 275 163 144 121 76
LAT (DEG N) 23.1 22.9 22.6 23.2 23.8 25.5 27.6 30.5 33.7 35.5 35.8 37.4 40.1
LONG(DEG W) 73.7 73.9 74.1 74.5 74.8 74.1 73.7 73.8 73.7 74.1 74.3 74.2 72.6
STM SPEED (KT) 4 3 3 7 7 10 13 15 13 6 4 11 14
HEAT CONTENT 56 57 37 57 26 59 55 27 13 7 1 0 0
FORECAST TRACK FROM OFCI INITIAL HEADING/SPEED (DEG/KT):220/ 5 CX,CY: -2/ -3
T-12 MAX WIND: 100 PRESSURE OF STEERING LEVEL (MB): 523 (MEAN=624)
GOES IR BRIGHTNESS TEMP. STD DEV. 50-200 KM RAD: 4.9 (MEAN=14.5)
% GOES IR PIXELS WITH T < -20 C 50-200 KM RAD: 100.0 (MEAN=65.0)
INDIVIDUAL CONTRIBUTIONS TO INTENSITY CHANGE
6 12 18 24 36 48 60 72 84 96 108 120
----------------------------------------------------------
SAMPLE MEAN CHANGE 1. 2. 3. 4. 6. 8. 9. 11. 12. 12. 13. 14.
SST POTENTIAL 0. 0. 1. 0. -3. -10. -20. -29. -38. -44. -49. -54.
VERTICAL SHEAR MAG -2. -4. -4. -3. -2. -2. 0. 0. 1. 0. -2. -2.
VERTICAL SHEAR ADJ -1. -2. -3. -4. -5. -6. -7. -8. -8. -7. -6. -5.
VERTICAL SHEAR DIR 0. 0. 1. 1. 1. 1. 2. 3. 5. 6. 8. 10.
PERSISTENCE 1. 1. 1. 0. 0. 0. 0. 0. 0. 0. 0. 0.
200/250 MB TEMP. 0. -1. -2. -2. -4. -6. -8. -11. -13. -16. -18. -20.
THETA_E EXCESS 0. 0. 0. 0. 0. 0. -1. -3. -6. -9. -12. -15.
700-500 MB RH 0. 0. 0. 0. -1. -1. -1. -1. -1. -1. -1. -1.
MODEL VTX TENDENCY 0. 1. 2. 1. 5. 8. 7. 8. 5. 5. 7. 5.
850 MB ENV VORTICITY 0. 1. 1. 2. 3. 5. 8. 10. 11. 12. 13. 13.
200 MB DIVERGENCE 0. 0. 0. 1. 2. 3. 3. 4. 3. 3. 2. 2.
850-700 T ADVEC 0. 0. 0. 0. 0. 0. 0. 0. -1. -2. -4. -7.
ZONAL STORM MOTION 0. 0. 0. 0. 0. 0. -1. -1. -1. -1. -2. -2.
STEERING LEVEL PRES 0. 0. 0. 0. 1. 1. 1. 1. 2. 1. 1. 1.
DAYS FROM CLIM. PEAK 0. 0. 0. 0. 0. 0. 0. 0. 0. 0. 0. 0.
GOES PREDICTORS 1. 2. 3. 4. 4. 4. 4. 3. 3. 2. 2. 2.
OCEAN HEAT CONTENT 0. 0. 0. 0. 0. 0. 0. 0. 0. 0. 0. 0.
----------------------------------------------------------
TOTAL CHANGE 1. 1. 2. 2. 5. 3. -6. -14. -28. -39. -48. -59.
** 2013 ATLANTIC RI INDEX AL112015 JOAQUIN 10/01/15 12 UTC **
( 30 KT OR MORE MAX WIND INCREASE IN NEXT 24 HR)
12 HR PERSISTENCE (KT): 10.0 Range:-49.5 to 33.0 Scaled/Wgted Val: 0.7/ 2.0
850-200 MB SHEAR (KT) : 9.3 Range: 28.8 to 2.9 Scaled/Wgted Val: 0.8/ 0.9
STD DEV OF IR BR TEMP : 4.9 Range: 37.5 to 2.9 Scaled/Wgted Val: 0.9/ 1.2
850-700 MB REL HUM (%): 68.2 Range: 43.2 to 93.5 Scaled/Wgted Val: 0.5/ 0.6
POT = MPI-VMAX (KT) : 32.4 Range: 28.4 to 139.1 Scaled/Wgted Val: 0.0/ 0.0
Heat content (KJ/cm2) : 46.6 Range: 0.0 to 155.1 Scaled/Wgted Val: 0.3/ 0.1
D200 (10**7s-1) : 48.0 Range:-23.1 to 181.5 Scaled/Wgted Val: 0.3/ 0.1
% area w/pixels <-30 C: 100.0 Range: 15.3 to 100.0 Scaled/Wgted Val: 1.0/ 0.2
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Re: ATL: JOAQUIN - Models
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Re: ATL: JOAQUIN - Models
Thanks Mark. I rarely post, but I'm here reading and learning a LOT. Its frustrating as someone wanting to learn more and more about tropical weather to have to weed through the "my model is better than your model!!!" threads.
cheers
Andy
cheers
Andy
tolakram wrote:Models are not a sport, and I honestly do not care what individuals think of the models. In my role as moderator I don't think these kinds of discussion add any value to this thread so I'm asking people to stop. Thanks.
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Re: ATL: JOAQUIN - Models
stormlover2013 wrote:http://www.ral.ucar.edu/hurricanes/realtime/plots/northatlantic/2015/al112015/track_gfs/aal11_2015100106_track_gfs.png
GFS ensembles
9 landfalling, 10 not
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Re: ATL: JOAQUIN - Models
stormlover2013 wrote:http://www.ral.ucar.edu/hurricanes/realtime/plots/northatlantic/2015/al112015/track_early/aal11_2015100112_track_early.png
Lmao.
We have our first Florida hit.
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- TreasureIslandFLGal
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Darn good thing that nobody has any faith in the CLIPper model. That scenario it shows would really not play out well for Florida if he just did a slow meander further southwest over the next 3 days and the front just fizzled away at its southern periphery as Joaquin pumped up the ridge to his northeast which allows him to miss the weakness connection to the north. Looks like the CLIP also doesn't let a full cutoff low form either, or immediately opens it back up. In any case, the time spent slowly drifting around south appears to show a missed connection with any supposed northern weakness through 72 hours. After that, who knows what could happen. Steering currents would remain weak I would suspect, or maybe 90L could eventual cause a weakness to the northeast to allow J to escape the trapping ridge. Then again, maybe with the front passage or disintegration, the ridge could ooze back west and cause J to continue a WSW drift until Hispanola ripped him up.
Of course, that meandering thought pattern was all pure conjecture based on the CLIP's read this morning....not that it will happen. Don't listen to me, follow NHC guidance, blah blah blah.
Of course, that meandering thought pattern was all pure conjecture based on the CLIP's read this morning....not that it will happen. Don't listen to me, follow NHC guidance, blah blah blah.

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Chrissy & Ligeia


Re: ATL: JOAQUIN - Models
Clipper isn't a model - based on climatology of storms in similar locations.
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- TreasureIslandFLGal
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agree ronjon that is isn't a true model taking into account as many minute factors, but in a way it still is, as it just looks at what storms have done in the past under similar broad based scenarios, and heading in the current direction a storm is heading. In this case, it shows a likely path based on: don't believe the cutoff low forms as expected by others. -as climatology rarely (if ever) would include that scenario having played out.
If other models start dropping the strong cutoff low scenario, it may prove a more accurate prediction. --but that is surely not the expectation, at least at this point in the game. But it can answer some people's "what if?" questions that I recently saw if the cutoff low doesn't form after all.
If other models start dropping the strong cutoff low scenario, it may prove a more accurate prediction. --but that is surely not the expectation, at least at this point in the game. But it can answer some people's "what if?" questions that I recently saw if the cutoff low doesn't form after all.

Last edited by TreasureIslandFLGal on Thu Oct 01, 2015 9:40 am, edited 1 time in total.
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Chrissy & Ligeia


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