Re: I'm wondering
Posted by Chris in Tampa on 9/29/2015, 9:56 pm
This could be complex. Please disregard what I previously said about impacts. Things are very uncertain and some models are extremely bullish on development. Euro is still offshore as of writing this though.

Lots of rain seems likely:
http://www.tropicaltidbits.com/analysis/models/?model=gfs&region=eus&pkg=apcpn&fh=240

But I am wondering about how large a system this could be later in the period:
http://www.tropicaltidbits.com/analysis/models/?model=gfs&region=eus&pkg=ir
I'm wondering how large it might be while still offshore. We could be talking about more than beach erosion. That is assuming it does pass near the coast or make a left turn into it.

I really wish real time data from the Integrated Kinetic Energy scale was still available from NOAA, such as the surge destructive potential. In 2014 NOAA gave that to a private company that charges you to see it. That was incredibly beneficial information with Sandy. Transferring it to a private company was ridiculous.

Cyclone phase analysis for 18Z run on Tuesday:
http://moe.met.fsu.edu/cyclonephase/gfs/fcst/archive/15092918/10.html
From: http://moe.met.fsu.edu/cyclonephase/

Then there is the really bullish intensity estimates from the GFDL and HWRF. Now that Joaquin has strengthened quite a bit fairly quickly, you have to start paying a lot more attention to them. (At 8pm the best track information had it at 70mph.)

Wide view HWRF: http://www.tropicaltidbits.com/analysis/models/?model=hwrf-p&region=11L&pkg=mslp_wind
Closeup: http://www.tropicaltidbits.com/analysis/models/?model=hwrf&region=11L&pkg=mslp_wind

Wide view GFDL: http://www.tropicaltidbits.com/analysis/models/?model=gfdl-p&region=11L&pkg=mslp_wind
Closeup: http://www.tropicaltidbits.com/analysis/models/?model=gfdl&region=11L&pkg=mslp_wind

Shear is forecast to lessen further. The SHIPS output below is based on the track at 0Z:
http://www.hurricanecity.com/models/data.cgi?basin=al&year=2015&storm=11&display=googlemap&latestrun=1&models=DSHP
(that link will display the latest track of the SHIPS model, the version that takes into account land interaction) At the moment later in the period that track is further away from the coast so it would take into account shear where the track is. Even if it got that right, if the storm is in a different place, shear would be different.


                   * ATLANTIC     SHIPS INTENSITY FORECAST          *
                   * IR SAT DATA AVAILABLE,       OHC AVAILABLE     *
                   *  JOAQUIN     AL112015  09/30/15  00 UTC        *

TIME (HR)          0     6    12    18    24    36    48    60    72    84    96   108   120
V (KT) NO LAND    60    64    67    70    73    76    79    83    87    91    92    90    77
V (KT) LAND       60    64    67    70    73    76    79    83    87    91    92    90    77
V (KT) LGE mod    60    66    71    75    78    82    83    85    91   100   102    89    74

Storm Type      TROP  TROP  TROP  TROP  TROP  TROP  TROP  TROP  TROP  TROP  TROP  TROP  TROP

SHEAR (KT)        18    17    21    20    18    13    11    10     6    10    24    29    23
SHEAR ADJ (KT)     5     4     2     2     6     9     8     0     1     8     5    -1     5
SHEAR DIR         13    14    21    31    30    31    23    21   334   283   239   220   220
SST (C)         29.9  29.9  29.9  29.9  29.8  29.8  29.8  29.8  29.8  29.6  28.3  27.8  27.6
POT. INT. (KT)   165   165   165   165   163   162   162   162   164   163   143   135   132
ADJ. POT. INT.   141   140   141   142   139   138   137   137   144   148   127   115   111
200 MB T (C)   -52.4 -52.5 -52.6 -52.1 -51.6 -51.7 -51.3 -51.2 -50.6 -50.4 -49.5 -48.8 -49.0
TH_E DEV (C)      10    10    10    11    11    10    11    10     9     8     7     6     6
700-500 MB RH     58    61    62    63    65    66    67    65    66    59    50    37    37
MODEL VTX (KT)    20    21    21    23    25    27    28    30    31    35    38    41    33
850 MB ENV VOR    23    15    20    33    39    54    80    95   126   148   197   245   181
200 MB DIV         0     9    19    14     2    19    30    61    67    81    65    48    35
700-850 TADV       0     0     0     0     2     2     6     6    14    11    35     5     8
LAND (KM)        665   639   611   569   527   466   418   426   515   653   579   447   521
LAT (DEG N)     25.8  25.7  25.6  25.4  25.2  24.9  24.6  24.7  25.4  27.4  30.5  33.0  34.6
LONG(DEG W)     71.5  71.9  72.3  72.7  73.2  73.9  74.4  74.5  74.0  73.5  73.0  72.0  70.3
STM SPEED (KT)     5     4     4     5     4     3     2     2     7    13    14    12    10
HEAT CONTENT      43    45    49    55    57    52    51    51    58    59    35    20    18

 FORECAST TRACK FROM OFCI      INITIAL HEADING/SPEED (DEG/KT):240/  5      CX,CY:  -3/ -1
 T-12 MAX WIND:  45            PRESSURE OF STEERING LEVEL (MB):  586  (MEAN=624)
 GOES IR BRIGHTNESS TEMP. STD DEV.  50-200 KM RAD:  16.2 (MEAN=14.5)
 % GOES IR PIXELS WITH T < -20 C    50-200 KM RAD:  78.0 (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          1.   2.   4.   5.   6.   6.   6.   6.   7.   6.   5.   3.
 VERTICAL SHEAR MAG     0.  -1.  -2.  -2.  -2.  -1.   1.   3.   4.   4.   2.   1.
 VERTICAL SHEAR ADJ     0.   0.  -1.  -1.  -2.  -3.  -4.  -4.  -4.  -4.  -3.  -3.
 VERTICAL SHEAR DIR     0.   0.   0.   0.   1.   1.   2.   2.   2.   3.   4.   5.
 PERSISTENCE            3.   4.   5.   5.   5.   5.   4.   4.   2.   1.   0.  -1.
 200/250 MB TEMP.       0.   0.  -1.  -1.  -2.  -3.  -4.  -5.  -7.  -9. -11. -13.
 THETA_E EXCESS         0.   0.   0.   0.   0.   0.   0.   0.  -1.  -2.  -3.  -4.
 700-500 MB RH          0.   0.   0.   0.  -1.  -1.  -2.  -2.  -2.  -2.  -1.  -1.
 MODEL VTX TENDENCY     0.   0.   1.   3.   5.   6.   8.   8.  12.  15.  16.   8.
 850 MB ENV VORTICITY   0.   0.   0.   0.   0.   1.   2.   3.   4.   6.   8.  10.
 200 MB DIVERGENCE      0.   0.   0.  -1.  -1.  -1.   0.   1.   1.   1.   1.   1.
 850-700 T ADVEC        0.   0.   0.   0.   0.   0.   0.   0.   0.   0.  -1.  -2.
 ZONAL STORM MOTION     0.   0.   0.   0.   0.   0.   0.   0.  -1.  -1.  -1.  -1.
 STEERING LEVEL PRES    0.   0.   0.   0.   0.   0.   0.   0.   0.   0.   0.   0.
 DAYS FROM CLIM. PEAK   0.   0.   0.   0.   0.   0.   0.   0.   0.   0.   0.   0.
 GOES PREDICTORS        0.   0.   1.   1.   1.   1.   1.   1.   1.   1.   1.   1.
 OCEAN HEAT CONTENT     0.   0.   0.   0.   0.   0.   0.   0.   0.   0.   0.   0.
                       ----------------------------------------------------------
 TOTAL CHANGE           4.   7.  10.  13.  16.  19.  23.  27.  31.  32.  30.  17.

  ** 2013 ATLANTIC RI INDEX AL112015 JOAQUIN    09/30/15  00 UTC **
          ( 30 KT OR MORE MAX WIND INCREASE IN NEXT 24 HR)

12 HR PERSISTENCE (KT):  15.0 Range:-49.5 to  33.0 Scaled/Wgted Val:  0.8/  2.2
850-200 MB SHEAR (KT) :  18.9 Range: 28.8 to   2.9 Scaled/Wgted Val:  0.4/  0.4
STD DEV OF IR BR TEMP :  16.2 Range: 37.5 to   2.9 Scaled/Wgted Val:  0.6/  0.8
850-700 MB REL HUM (%):  70.0 Range: 43.2 to  93.5 Scaled/Wgted Val:  0.5/  0.7
POT = MPI-VMAX (KT)   :  80.8 Range: 28.4 to 139.1 Scaled/Wgted Val:  0.5/  0.3
Heat content (KJ/cm2) :  49.8 Range:  0.0 to 155.1 Scaled/Wgted Val:  0.3/  0.1
D200 (10**7s-1)       :   8.8 Range:-23.1 to 181.5 Scaled/Wgted Val:  0.2/  0.1
% area w/pixels <-30 C:  72.0 Range: 15.3 to 100.0 Scaled/Wgted Val:  0.7/  0.1

Prob of RI for 25 kt RI threshold=    20% is   1.7 times the sample mean(11.9%)
Prob of RI for 30 kt RI threshold=    12% is   1.6 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=     6% is   1.9 times the sample mean( 3.0%)

  ##         ANNULAR HURRICANE INDEX (AHI) AL112015 JOAQUIN    09/30/15  00 UTC         ##
  ## STORM NOT ANNULAR, SCREENING STEP FAILED, NPASS=3 NFAIL=4                          ##
  ## 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 AL112015 JOAQUIN    09/30/2015  00 UTC **
TIME(HR)   0-12  12-24(0-24)  24-36(0-36)  36-48(0-48)
CLIMO(%)     0      3(  3)       4(  7)       5( 12)     <-- PROB BASED ON INTENSITY ONLY
PROB(%)      0      0(  0)       0(  0)       0(  0)     <-- FULL MODEL PROB (RAN NORMALLY)


Latest SHIPS output: http://ftp.nhc.noaa.gov/atcf/stext/

About LGEM (LGE mod) intensity: http://www.nhc.noaa.gov/modelsummary.shtml
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Tropical Storm JOAQUIN - AquaRN, 9/28/2015, 11:09 pm
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