********************************************************************************

1873/01:  No major changes from Partagas and Diaz (1995b).  Track 
unaltered from Neumann et al. (1993).  Inland decay model of Kaplan 
and DeMaria (1995) utilized for inland winds over Georgia.  The best 
track provided appears to describe the full life cycle of this tropical 
cyclone (from its formation as a tropical storm until its dissipation 
below tropical depression strength).

********************************************************************************

1873/02: No major changes from Partagas and Diaz (1995b), who made
large alterations to the track shown in Neumann et al. (1993).  These
track changes are found to be reasonable.  962 mb central pressure 
suggests 88 kt from the northern wind-pressure relationship - 90 kt used 
in best track.  Storm is determined to have reached major hurricane 
status for the two days before the above central pressure measurement 
was made at latitude 44N.  The best track provided appears to describe 
the full life cycle of this tropical cyclone (from its formation as a 
tropical storm to its peak as a major hurricane until its dissipation as 
an extratropical cyclone).  

1873/02 - 2003 REVISION:

04550 08/13/1873 M=16  2 SNBR= 147 NOT NAMED   XING=0 SSS=0
04550 08/13/1873 M=16  2 SNBR= 150 NOT NAMED   XING=0 SSS=0
                               ***

04555 08/13*139 250  40    0*140 260  40    0*140 270  40    0*141 281  40    0
04560 08/14*141 293  50    0*142 306  50    0*143 320  50    0*144 330  50    0
04565 08/15*145 344  50    0*145 359  50    0*145 373  50    0*146 384  50    0
04570 08/16*147 397  60    0*148 412  60    0*150 427  60    0*153 440  60    0
04575 08/17*156 455  70    0*160 470  70    0*165 490  70    0*169 505  70    0
04580 08/18*175 520  70    0*182 536  70    0*187 550  70    0*195 564  70    0
04585 08/19*202 579  80    0*212 595  80    0*220 610  80    0*229 621  80    0
04590 08/20*239 635  80    0*249 646  80    0*260 656  80    0*268 666  80    0
04595 08/21*278 673  90    0*290 678  90    0*303 683  90    0*310 684  90    0
04595 08/21*278 673  90    0*290 678  90    0*303 682  90    0*310 684  90    0
                                                  ***

04600 08/22*317 685  90    0*325 686  90    0*333 685  90    0*343 683  90    0
04605 08/23*352 680 100    0*360 676 100    0*370 670 100    0*383 664 100    0
04610 08/24*395 658 100    0*409 646 100    0*420 635  90    0*430 614  90    0
04615 08/25*437 589  90  962*444 566  90    0*450 550  80    0*457 543  80    0
04620 08/26*460 541  80    0*465 541  80    0*470 540  70    0*474 540  70    0
04625 08/27*478 539  70    0*482 537  70    0E485 535  60    0E494 526  60    0
04630 08/28E504 513  60    0E510 498  60    0E520 480  50    0E530 460  50    0
04635 HR

Minor track alteration on the 21st for more realistic motion.

********************************************************************************

1873/03:  No major changes from Partagas and Diaz (1995b), who made
reasonable small alterations to the track shown in Neumann et al. (1993).
Pressure reading of 992 mb not in hurricane's center (at 12 UTC, 19th of 
September) suggests winds of at least 59 kt from the Gulf of Mexico wind-
pressure relationship - 70 kt chosen for best track.  Inland decay 
model of Kaplan and DeMaria (1995) utilized for inland winds over the 
SE United States.  Storm is determined to have reached hurricane force
in the Gulf of Mexico based upon destruction that occurred in Tallahassee,
Florida; storm regained hurricane strength in the Atlantic based upon above
peripheral surface pressure report along with several ship observations.

********************************************************************************

1873/04:  No major changes from Partagas and Diaz (1995b).  Track 
unaltered from Neumann et al. (1993).  Inland decay model of Kaplan 
and DeMaria (1995) utilized for inland winds over Florida.

********************************************************************************

1873/05:  No major changes from Partagas and Diaz (1995b), who made
large alterations to the track reasonably shown in Neumann et al. 
(1993).  These track changes are found to be reasonable.  Inland decay 
model of Kaplan and DeMaria (1995) utilized for inland winds over 
Hispanola, Cuba and the SE United States.  Used an accelerated decay 
rate over Cuba to account for enhanced topography.  Pressure reading 
of 969 mb not in hurricane's center (on 12 UTC, September 28th) suggests 
winds of at least 91 kt from the southern wind-pressure relationship -
100 kt chosen for best track.  Pressure reading of 971 mb not
in hurricane's center (on 00 UTC, September 29th) suggests winds of
at least 88 kt - 90 kt chosen for best track.  Estimate of 959 mb for
central pressure at landfall in SW Florida from Ho (1989) appears
reasonable and matches SLOSH modeling work by Jarvinen (1990).
959 mb central pressure suggests 101 kt from the Gulf of Mexico
wind-pressure relationship - 100 kt chosen for the best track.  Storm tide
value of 14' at Punta Rassa, Florida from Partagas and Diaz (1995b).  Storm
is determined to have reached major hurricane status on the 28th of
September based upon peripheral surface pressure reading of 969 mb and
destruction that occurred in Jacmal, Haiti.  Storm regained major
hurricane status on the 7th of October based upon the estimate of central 
pressure of 959 mb and surge/destruction in Punta Rassa.

1873/05 - 2003 REVISION:

04690 09/26/1873 M=15  5 SNBR= 150 NOT NAMED   XING=1 SSS=3
04690 09/26/1873 M=15  5 SNBR= 153 NOT NAMED   XING=1 SSS=3
                               ***

04695 09/26*147 623  40    0*148 631  40    0*150 640  50    0*153 651  50    0
04700 09/27*157 665  60    0*160 676  60    0*162 690  70    0*166 701  70    0
04705 09/28*169 711  80    0*174 723  90    0*180 730 100    0*190 739  90    0
04710 09/29*197 745  90    0*202 755  80    0*202 765  60    0*202 771  50    0
04715 09/30*201 778  40    0*200 784  40    0*200 790  40    0*201 796  40    0
04720 10/01*201 801  40    0*201 806  40    0*200 810  40    0*200 814  40    0
04725 10/02*200 818  50    0*200 821  50    0*200 825  50    0*200 828  50    0
04730 10/03*200 831  60    0*200 836  60    0*200 840  70    0*200 846  70    0
04735 10/04*200 851  70    0*201 856  70    0*202 860  80    0*206 861  80    0
04735 10/04*200 851  70    0*201 856  70    0*202 860  80    0*204 861  80    0
                                                               ***

04740 10/05*210 864  80    0*212 865  80    0*215 865  90    0*219 864  90    0
04740 10/05*208 864  80    0*212 865  80    0*215 865  90    0*219 864  90    0
            ***

04745 10/06*224 861  90    0*230 859  90    0*237 855 100    0*247 841 100    0
04750 10/07*262 825 100  959*281 803  80    0*297 786  80    0*311 771  80    0
04755 10/08*324 756  90    0*337 741  90    0*350 726  80    0*363 709  80    0
04760 10/09*375 685  70    0*388 661  70    0E395 645  60    0E400 630  60    0
04765 10/10E405 615  60    0E410 600  60    0*  0   0   0    0*  0   0   0    0
04770 HRBFL3CFL2DFL1    

Track slightly altered to provide a more realistic motion.

********************************************************************************