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

1882/01:  No major changes from this newly documented hurricane
by Partagas and Diaz (1996).  Storm is determined to have reached hurricane
intensity based upon reports from the ships "Case" and "Ida".

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

1882/02:  No major changes from Partagas and Diaz (1996), who made large
alterations to the track shown in Neumann et al. (1993), originally storm
number 1.  These track changes are found to be reasonable.  981 mb central 
pressure suggests winds of 76 kt from the southern wind-pressure 
relationship - 80 kt chosen for best track.  961 mb central pressure 
corresponds to 94 kt from the subtropical latitude wind-pressure 
relationship - 90 kt chosen for best track.  949 mb central pressure 
corresponds to 103 kt from the subtropical wind-pressure relationship - 
100 kt chosen for best track.  1000 mb central pressure suggests 49 kt 
from the northern wind-pressure relationship - 50 kt chosen for best track.  
A pressure reading of 980 mb not in the hurricane's center (at 06 UTC on 
the 4th of September) suggests winds of at least 78 kt from the southern 
wind-pressure relationship - 80 kt chosen for the best track.  A pressure 
reading of 986 mb not in the hurricane's center (at 18 UTC on the 5th) 
suggests winds of at least 70 kt from the southern wind-pressure 
relationship - 70 kt chosen for the best track.  Inland decay model of 
Kaplan and DeMaria (1995) utilized for inland winds over the S.E. United 
States.  Storm is determined to have reached major hurricane intensity 
based upon central pressure reading of 949 mb from the ship "Cato" while 
over the Gulf of Mexico.

1882/02 - 2003 REVISION:

07485 09/02/1882 M=12  2 SNBR= 216 NOT NAMED   XING=1 SSS=3
07485 09/02/1882 M=12  2 SNBR= 219 NOT NAMED   XING=1 SSS=3
                               ***

07490 09/02*195 675  50    0*197 685  50    0*202 693  50    0*207 701  50    0
07495 09/03*212 709  60    0*217 718  60    0*220 725  70    0*222 734  70    0
07500 09/04*225 743  80    0*225 751  80    0*225 761  80    0*224 770  80    0
07500 09/04*225 743  80    0*225 751  80    0*225 761  90    0*224 770  90    0
                                                       **               **

07505 09/05*224 778  80    0*222 786  80    0*222 795  80    0*222 809  70    0
07505 09/05*224 778  90    0*224 786  80    0*224 795  80    0*224 809  70    0
                     **      ***              ***              ***

07510 09/06*222 820  70    0*222 829  70    0*222 838  70    0*222 846  70    0
07510 09/06*224 820  70    0*224 829  70    0*224 838  70    0*224 846  70    0
            ***              ***              ***              ***

07515 09/07*225 858  80  981*231 866  80    0*237 873  80    0*242 876  80    0
07515 09/07*226 858  80  981*231 866  80    0*237 873  80    0*242 876  80    0
            ***

07520 09/08*247 880  90    0*254 883  90    0*260 886  90    0*264 886  90    0
07520 09/08*247 880  90    0*254 883  90    0*260 886  90    0*264 887  90    0
                                                                   ***

07525 09/09*268 888  90    0*273 886  90    0*277 884  90    0*288 880  90  961
07525 09/09*268 888  90    0*272 887  90    0*277 884  90    0*288 880  90  961
                             *** ***

07530 09/10*300 871 100  949*311 861  80    0*319 851  60    0*330 841  40    0
07535 09/11*337 833  40    0*345 821  40    0*353 808  40    0*367 783  40    0
07540 09/12*384 749  50    0*400 715  60    0*417 681  50 1000*437 645  50    0
07545 09/13E452 610  40    0E465 575  40    0*  0   0   0    0*  0   0   0    0
07550 HRAFL3 AL1

Re-analysis effort by Perez (2000) has analyzed this hurricane as a 
Category 2 landfall in Cuba, instead of a Category 1 assigned in HURDAT.
Winds are adjusted accordingly on the 4th and 5th.  Perez' track was slightly 
farther north on the 5th and 6th, so the latitudes on those dates have also 
been changed accordingly.  Track altered slightly on the 8th and 9th to
provide a more realistic translational velocity.

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

1882/03 - 2003 ADDITION:

07566 09/14/1882 M= 3  3 SNBR= 220 NOT NAMED   XING=1 SSS=2
07567 09/14*280 890  90    0*282 900  90    0*285 910  90    0*289 920  90    0
07568 09/15*294 930  90    0*299 938  80    0*304 945  60    0*309 950  40    0
07569 09/16*315 953  30    0*  0   0   0    0*  0   0   0    0*  0   0   0    0
07570 HR LA2CTX1

Roth (1997a,b) documents a newly described system that made landfall
along the U.S. coastline near the Texas-Louisiana border:

"A strong tropical storm hit the mouth of the Sabine River. A "terrific wind 
 and rain storm" caused damage to homes in Sabine Pass, Tx. The Lake Charles 
 Echo, La. reported it as a "hurricane" that destroyed a house and injured 
 its occupant.  Streets in town were covered by 3 feet of water. Fences were 
 blown over a mile from their previous location.  That night [the 14th], a 
 "Hard wind and rain" visited Lake Charles, described as a lively gale". Port 
 Eads, La. had winds of 70 m.p.h. and a pressure of 29.38". Abbeville, La. 
 reported no damage with the storm."

From this description a rough track of the storm was created that goes
from southeast to northwest, making landfall just east of Sabine Pass.
Storm surge modeling (B. Jarvinen, personal communication) suggests that
3' of standing water in the streets of Lake Charles requires a Category 2
at landfall.  Thus this system is estimated as 90 kt at landfall.  The 
inland decay model of Kaplan and DeMaria (1995) utilized for inland winds 
over Texas and Louisiana. 

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

1882/04:  No major changes from Partagas and Diaz (1996), (was originally 
storm #3 in the Partagas and Diaz report).  Track unaltered from Neumann 
et al. (1993), their storm number 2.  1005 mb central pressure corresponds 
to 40 kt from the northern wind-pressure relationship, which is utilized 
as the best track intensity value.  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 storm intensity).

1882/04 - 2003 REVISION:

07570 09/21/1882 M= 4  3 SNBR= 218 NOT NAMED   XING=1 SSS=0
07570 09/21/1882 M= 4  4 SNBR= 218 NOT NAMED   XING=1 SSS=0
                       *

07575 09/21*285 768  40    0*292 771  40    0*300 775  40    0*308 776  40    0
07580 09/22*315 776  40    0*322 776  40    0*330 774  50    0*340 771  50    0
07580 09/22*315 776  40    0*322 776  40    0*330 775  50    0*340 773  50    0
                                                  ***              ***

07585 09/23*350 770  40    0*360 766  40 1005*370 761  40    0*382 755  40    0
07590 09/24*394 745  40    0*410 725  40    0*  0   0   0    0*  0   0   0    0
07595 TS    

Track altered slightly on the 22nd to provide a more realistic smooth track.  

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

1882/05:  No major changes from this newly documented hurricane from
Partagas and Diaz (1996), (was originally storm #4 in the Partagas
and Diaz report).  Storm is determined to have reached hurricane
intensity based upon reports from the ships "R.A. Allen" and "Sedmi
Dubrovacki".

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

1882/06:  No major changes from Partagas and Diaz (1996), (was originally 
storm #5 in the Partagas and Diaz report).  Track unaltered from Neumann 
et al. (1993), their storm number 3.  975 mb central pressure corresponds 
to 84 kt in the southern wind-pressure relationship - 90 kt chosen for 
best track.  981 mb central pressure corresponds to 76 kt of sustained 
winds from the southern wind-pressure relationship - 80 kt utilized in 
best track.  Inland decay model of Kaplan and DeMaria (1995) utilized for 
inland winds over Florida and Georgia.  Storm is determined to have been 
of hurricane intensity while in the Caribbean and Gulf of Mexico based 
upon these central pressure readings, ship reports and a 9 foot storm 
tide experienced at the mouth of the Colona River, Cuba.  Storm regained 
hurricane intensity while over the Atlantic based upon several ship 
reports.

07620 10/05/1882 M=11  5 SNBR= 219 NOT NAMED   XING=1 SSS=1
07620 10/05/1882 M=11  6 SNBR= 223 NOT NAMED   XING=1 SSS=1
                       *       ***

07625 10/05*142 816  40    0*146 819  40    0*150 820  40    0*154 821  40    0
07630 10/06*158 821  50    0*162 823  50    0*166 824  50    0*170 825  50    0
07635 10/07*172 826  60    0*177 828  60    0*180 829  70    0*184 830  70    0
07640 10/08*187 831  80    0*191 831  80    0*195 831  90    0*202 835  90    0
07640 10/08*187 831  80    0*191 832  90    0*195 833 100    0*202 835 110    0
                                 ***  **          *** ***              ***

07645 10/09*212 836  90  975*222 839  80  981*235 840  80    0*244 840  80    0
07645 10/09*212 837 120    0*222 839 100    0*235 840  90    0*244 841  80    0
                *** ***  ***         ***  ***          **          ***

07650 10/10*254 841  70    0*265 841  70    0*275 840  70    0*283 838  70    0
07655 10/11*291 836  70    0*298 831  60    0*305 826  50    0*312 815  50    0
07660 10/12*320 804  60    0*330 790  60    0*338 775  70    0*342 760  70    0
07665 10/13*347 748  70    0*350 733  70    0*355 720  70    0*358 711  70    0
07670 10/14*360 704  70    0*362 696  70    0*365 690  70    0*367 683  70    0
07675 10/15*370 676  60    0*372 670  60    0*375 661  60    0*378 651  60    0
07680 HRAFL1

Re-analysis effort by Perez (2000) has analyzed this hurricane as a 
Category 4 landfall in Cuba, instead of a Category 2 assigned in HURDAT.
The pressure values of 975 mb and 981 mb on 00 and 06Z on the 9th are
found to be peripheral pressures, instead of central pressures based upon
additional information provided by Perez (2000).  Winds are adjusted 
accordingly on the 4th and 5th.

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