ATL: NINE - Models
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- cycloneye
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ATL: NINE - Models
Only models here.
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Hmm maybe this system could be the next 'cane!
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Okay guys, just because I want to BE a meteorologist, want to go to school for meteorology, DOES NOT MAKE ME A METEOROLOGIST. Anything I say about tropical weather is either me learning something new, or is just an opinion and nothing more than that. I can almost guarantee you that I will be wrong about pretty much everything.
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That is some weird path models. Some of those have some SHARP turns lol
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Okay guys, just because I want to BE a meteorologist, want to go to school for meteorology, DOES NOT MAKE ME A METEOROLOGIST. Anything I say about tropical weather is either me learning something new, or is just an opinion and nothing more than that. I can almost guarantee you that I will be wrong about pretty much everything.
- Hurricaneman
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Re: ATL: INVEST 93L - Models
Sanibel wrote:Sharp turn right?
almost all the models have that sharp turn due to the low to its north around 25N
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- cycloneye
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Re: ATL: INVEST 93L - Models
Pretty intense.
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- cycloneye
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Re: ATL: INVEST 93L - Models
Intense hurricane if models are right.
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I'm not surprised the Euro is backing off on development (and I'll believe a weak Euro solution over a strong GFS one given the latter's equally terrible history) as this system is really a mess at the surface. It seems to be a very elongated trough, with winds simply flowing directly from one low pressure area to another. I don't see anything beyond just being strong ITCZ activity.
Last edited by Hammy on Sun Sep 13, 2015 2:45 pm, edited 1 time in total.
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Re: ATL: INVEST 93L - Models
Shear will not be a big problem in the short to medium term.
Code: Select all
* ATLANTIC SHIPS INTENSITY FORECAST *
* IR SAT DATA AVAILABLE, OHC AVAILABLE *
* INVEST AL932015 09/13/15 18 UTC *
TIME (HR) 0 6 12 18 24 36 48 60 72 84 96 108 120
V (KT) NO LAND 25 30 36 42 47 59 68 76 80 80 78 80 85
V (KT) LAND 25 30 36 42 47 59 68 76 80 80 78 80 85
V (KT) LGE mod 25 28 32 36 41 52 66 79 87 84 78 74 70
Storm Type TROP TROP TROP TROP TROP TROP TROP TROP TROP TROP TROP TROP TROP
SHEAR (KT) 14 12 13 13 14 8 10 10 13 18 20 23 19
SHEAR ADJ (KT) -3 -5 -6 -5 -10 -6 -3 4 9 14 8 2 -3
SHEAR DIR 37 39 43 60 77 27 359 323 311 277 262 263 246
SST (C) 28.2 28.2 28.1 28.1 28.1 28.2 28.3 28.2 27.9 27.7 27.8 27.8 27.8
POT. INT. (KT) 139 140 138 137 137 138 139 138 136 134 136 137 137
ADJ. POT. INT. 139 140 136 135 134 132 133 132 130 130 131 130 127
200 MB T (C) -53.1 -53.4 -53.5 -53.4 -53.3 -53.7 -53.5 -54.0 -53.4 -53.8 -54.0 -54.5 -54.5
TH_E DEV (C) 7 7 7 8 9 9 9 8 7 7 7 7 6
700-500 MB RH 68 69 69 66 62 59 56 63 66 70 69 67 65
MODEL VTX (KT) 11 13 13 15 15 16 15 15 17 18 19 23 28
850 MB ENV VOR 44 49 48 47 44 32 23 34 19 9 -4 -25 -20
200 MB DIV 46 49 12 -26 -31 -18 14 79 83 73 69 80 86
700-850 TADV -13 -12 -11 -10 -6 -1 0 3 4 13 17 30 26
LAND (KM) 1855 1758 1664 1592 1523 1436 1447 1516 1693 1943 2266 2138 1990
LAT (DEG N) 10.3 10.5 10.7 10.9 11.1 11.6 12.6 13.7 15.5 17.7 20.6 23.8 27.0
LONG(DEG W) 35.5 36.6 37.6 38.4 39.3 40.6 41.3 41.5 41.1 40.2 39.1 37.7 35.8
STM SPEED (KT) 9 11 9 9 8 6 6 7 11 14 16 18 18
HEAT CONTENT 27 25 24 22 18 13 9 7 6 9 21 15 9
FORECAST TRACK FROM BAMM INITIAL HEADING/SPEED (DEG/KT):275/ 8 CX,CY: -7/ 1
T-12 MAX WIND: 20 PRESSURE OF STEERING LEVEL (MB): 537 (MEAN=624)
GOES IR BRIGHTNESS TEMP. STD DEV. 50-200 KM RAD: 9.8 (MEAN=14.5)
% GOES IR PIXELS WITH T < -20 C 50-200 KM RAD: 96.0 (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. 2. 6. 11. 17. 22. 26. 29. 31. 32.
VERTICAL SHEAR MAG 1. 2. 2. 3. 4. 5. 5. 5. 3. 2. 0. -1.
VERTICAL SHEAR ADJ 0. 1. 1. 2. 3. 4. 4. 3. 1. 0. 0. 0.
VERTICAL SHEAR DIR 1. 2. 3. 4. 7. 9. 10. 10. 9. 8. 8. 7.
PERSISTENCE 1. 1. 2. 2. 2. 2. 2. 1. 1. 1. 0. 0.
200/250 MB TEMP. 0. 0. 0. 0. 0. 0. 1. 1. 1. 2. 3. 4.
THETA_E EXCESS 0. -1. -1. -1. -2. -2. -3. -4. -5. -7. -8. -9.
700-500 MB RH 0. 0. 0. -1. -1. -1. -2. -2. -2. -2. -2. -2.
MODEL VTX TENDENCY 0. 1. 2. 2. 3. 2. 2. 4. 5. 5. 8. 12.
850 MB ENV VORTICITY 0. 0. 0. 1. 1. 1. 1. 1. 1. 0. 0. -1.
200 MB DIVERGENCE 0. 0. 0. -1. -1. -2. -1. 0. 1. 1. 1. 1.
850-700 T ADVEC 0. 0. 0. 0. 0. 0. 0. 0. 0. 0. 0. -1.
ZONAL STORM MOTION 0. 0. 0. 0. 1. 1. 1. 1. 1. 1. 1. 1.
STEERING LEVEL PRES 0. 0. 0. 0. 1. 1. 1. 1. 1. 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. 3. 2. 1. 1. 1. 2.
OCEAN HEAT CONTENT 0. 0. 0. 0. 0. 0. 0. 0. 0. 0. 0. 0.
----------------------------------------------------------
TOTAL CHANGE 5. 11. 17. 22. 34. 43. 51. 55. 55. 53. 55. 60.
** 2013 ATLANTIC RI INDEX AL932015 INVEST 09/13/15 18 UTC **
( 30 KT OR MORE MAX WIND INCREASE IN NEXT 24 HR)
12 HR PERSISTENCE (KT): 5.0 Range:-49.5 to 33.0 Scaled/Wgted Val: 0.7/ 1.9
850-200 MB SHEAR (KT) : 13.3 Range: 28.8 to 2.9 Scaled/Wgted Val: 0.6/ 0.7
STD DEV OF IR BR TEMP : 9.8 Range: 37.5 to 2.9 Scaled/Wgted Val: 0.8/ 1.0
850-700 MB REL HUM (%): 65.8 Range: 43.2 to 93.5 Scaled/Wgted Val: 0.4/ 0.6
POT = MPI-VMAX (KT) : 111.9 Range: 28.4 to 139.1 Scaled/Wgted Val: 0.8/ 0.5
Heat content (KJ/cm2) : 23.2 Range: 0.0 to 155.1 Scaled/Wgted Val: 0.1/ 0.0
D200 (10**7s-1) : 10.0 Range:-23.1 to 181.5 Scaled/Wgted Val: 0.2/ 0.1
% area w/pixels <-30 C: 92.0 Range: 15.3 to 100.0 Scaled/Wgted Val: 0.9/ 0.2
Prob of RI for 25 kt RI threshold= 28% is 2.3 times the sample mean(11.9%)
Prob of RI for 30 kt RI threshold= 13% is 1.7 times the sample mean( 7.6%)
Prob of RI for 35 kt RI threshold= 7% is 1.5 times the sample mean( 4.6%)
Prob of RI for 40 kt RI threshold= 5% is 1.8 times the sample mean( 3.0%)
## ANNULAR HURRICANE INDEX (AHI) AL932015 INVEST 09/13/15 18 UTC ##
## STORM NOT ANNULAR, SCREENING STEP FAILED, NPASS=4 NFAIL=3 ##
## AHI= 0 (AHI OF 100 IS BEST FIT TO ANN. STRUC., 1 IS MARGINAL, 0 IS NOT ANNULAR) ##
** PROBLTY OF AT LEAST 1 SCNDRY EYEWL FORMTN EVENT AL932015 INVEST 09/13/2015 18 UTC **
TIME(HR) 0-12 12-24(0-24) 24-36(0-36) 36-48(0-48)
CLIMO(%) 0 0( 0) 0( 0) 0( 0) <-- PROB BASED ON INTENSITY ONLY
PROB(%) 0 0( 0) 0( 0) 0( 0) PC4 UNAVAIL...MODEL SKILL DEGRADED
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GFS out to 138 hours, significantly weaker than last run, 15mb difference in pressure (965 vs 980)
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- TropicalAnalystwx13
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Re:
Hammy wrote:I'm not surprised the Euro is backing off on development (and I'll believe a weak Euro solution over a strong GFS one given the latter's equally terrible history) as this system is really a mess at the surface. It seems to be a very elongated trough, with winds simply flowing directly from one low pressure area to another. I don't see anything beyond just being strong ITCZ activity.
Why would a system's current structure preclude eventual significant strengthening? The GFS doesn't say this will be a major hurricane tomorrow.
As Alyono said, this is likely our next hurricane, and it has at least some potential to be our next major hurricane.
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Re: Re:
TropicalAnalystwx13 wrote:Hammy wrote:I'm not surprised the Euro is backing off on development (and I'll believe a weak Euro solution over a strong GFS one given the latter's equally terrible history) as this system is really a mess at the surface. It seems to be a very elongated trough, with winds simply flowing directly from one low pressure area to another. I don't see anything beyond just being strong ITCZ activity.
Why would a system's current structure preclude eventual significant strengthening? The GFS doesn't say this will be a major hurricane
Very often the models have difficulty with less organized systems and have a bad tendency to overdevelop them. And far too often I've seen systems that are forecast to develop when they are in a setup like this but don't--there are two very strong waves fairly close together and that generally leads to neither developing since one can't get organized while being so close to the other.
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- cycloneye
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Re: ATL: INVEST 93L - Models
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- Gustywind
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Re: Re:
Hammy wrote:TropicalAnalystwx13 wrote:Hammy wrote:I'm not surprised the Euro is backing off on development (and I'll believe a weak Euro solution over a strong GFS one given the latter's equally terrible history) as this system is really a mess at the surface. It seems to be a very elongated trough, with winds simply flowing directly from one low pressure area to another. I don't see anything beyond just being strong ITCZ activity.
Why would a system's current structure preclude eventual significant strengthening? The GFS doesn't say this will be a major hurricane
Very often the models have difficulty with less organized systems and have a bad tendency to overdevelop them. And far too often I've seen systems that are forecast to develop when they are in a setup like this but don't--there are two very strong waves fairly close together and that generally leads to neither developing since one can't get organized while being so close to the other.
Interresting point of vue Hammy .
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- gatorcane
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There is a big difference between the ECMWF and GFS here as the ECMWF for the past couple of runs shows no development of this wave while the GFS eventually develops this into a hurricane.
Look at the big difference in the 5-day forecast between these two models:
GFS with a hurricane recurving:
ECMWF with a 1012MB low moving more WNW with the low-level flow
Look at the big difference in the 5-day forecast between these two models:
GFS with a hurricane recurving:
ECMWF with a 1012MB low moving more WNW with the low-level flow
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GFS back to strong Cat 2 at 144 hours (but seems weaker with later system)
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- cycloneye
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Re: ATL: INVEST 93L - Models
Models have reversed on intensity for now.Even SHIP that had a hurricane stays as a 60kt storm.
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