Preliminary Report
Hurricane Floyd
7 - 17 September, 1999

Richard J. Pasch, Todd B. Kimberlain and Stacy R. Stewart
National Hurricane Center
18 November 1999

Floyd was a large and intense Cape Verde hurricane that pounded the central and northern Bahama islands, seriously threatened Florida, struck the coast of North Carolina and moved up the United States east coast into New England. It neared the threshold of category five intensity on the Saffir/Simpson Hurricane Scale as it approached the Bahamas, and produced a flood disaster of immense proportions in the eastern United States, particularly in North Carolina.

a. Synoptic History

Floyd can be traced back to a tropical wave that emerged from western Africa on 2 September. This system was not particularly impressive-looking, in terms of the organization of the convection shown on satellite images, but there was evidence of curvature in the cloud lines. Overall the system was broad and disorganized, yet easily recognizable as a synoptic-scale entity.

The wave proceeded westward across the eastern tropical Atlantic at about the normal speed of propagation, 6 degrees of longitude per day, with little apparent change, for several days. A center of circulation was estimated late on 5 September near 15N 32.5W but the cloud pattern lacked sufficient deep convection for a Dvorak classification. On 6 September, there was enough of a curved band of deep convection present so that the system was classified as a T1.0 on the Dvorak scale around 1200 UTC. A favorable upper-level outflow pattern existed over the area, and the cloud pattern became more consolidated and better organized on the 7th. Tropical Depression Eight formed about 1000 miles east of the Lesser Antilles by 1800 UTC that day.

A deep-layer ridge prevailed to the north of the cyclone and the associated steering current moved the system west-northwestward at 12-15 knots for a couple of days. When it reached a position about 750 n mi east of the Leeward Islands, the cloud pattern became sufficiently well organized for the system to become Tropical Storm Floyd around 0600 UTC 8 September. Even though large-scale conditions appeared conducive for strengthening, there was a lack of a well-defined inner core. This was evidenced by visible, infrared, and microwave imagery that showed no tightly curved banding features or a concentration of deep convection close to the center, a condition that probably prevented rapid intensification during the early stages of the tropical cyclone. Floyd slowly strengthened and became a hurricane by 1200 UTC 10 September while centered about 200 n mi east-northeast of the northern Leeward Islands.

As Floyd was nearing hurricane status, a mid-tropospheric trough in the vicinity of 60-65W longitude caused a slowing of the forward speed, and then a turn toward the northwest. The northwestward motion continued until the 11th, keeping the hurricane well to the northeast of the islands of the northeastern Caribbean. On the 11th, Floyd neared the southwest portion of the mid-Atlantic upper-tropospheric trough which was situated to the north of Puerto Rico, i.e. close to its climatological position. Historically, hurricanes have had difficulty strengthening in this area. Floyd's upper-level outflow was disrupted over the southern semicircle by the trough and an anticyclone over the eastern Caribbean. Consequently, after strengthening nearly to category three status early on the 11th, the hurricane weakened to 85 knots around 0000 UTC on the 12th. Early on the 12th, rising mid- to upper-tropospheric heights to the north of Floyd forced a turn toward the west. The westward turn also marked the beginning of a major strengthening episode (this phenomenon has also been observed with many past hurricanes, e.g. Andrew of 1992). Maximum sustained winds increased from 95 knots to 135 knots, and the central pressure fell about 40 mb from early on the 12th to early on the 13th. From 0600 to 1800 on the 13th, Floyd was at the top end of category four intensity on the Saffir/Simpson Hurricane Scale.

One potential contributor to the significant strengthening of Floyd was the presence of enhanced upper oceanic heat content along its track. Analyses from the Physical Oceanography Division of NOAA/AOML showed relatively high values of heat content just to the east of the Bahamas a day or two before Floyd passed through the area.

Floyd was aimed at the central Bahamas until late on the 13th, when the heading became west-northwestward. The eye passed just 20 to 30 n mi northeast and north of San Salvador and Cat Islands on the night of the 13th. Floyd's eyewall passed over central and northern Eleuthera on the morning of the 14th, and after turning toward the northwest, Floyd struck Abaco island on the afternoon of the 14th. By the time the hurricane hit Abaco, it had weakened somewhat from its peak, but Floyd was still a borderline category three/four hurricane.

As a mid- to upper-tropospheric trough over the eastern United States eroded the subtropical ridge over the extreme western Atlantic, Floyd continued to turn gradually to the right. The center of the hurricane paralleled the central Florida coast, passing about 95 n mi east of Cape Canaveral around 0900 UTC 15 September. By the afternoon of the 15th, Floyd was abeam of the Florida/Georgia border and headed northward toward the Carolinas.

Although there was a fluctuation in intensity, related to an eyewall replacement event discussed in the next section, overall the intensity of Floyd diminished from the 13th to the 15th. Environmental causes for intensity change are not entirely understood, but two large-scale factors probably contributed to a gradual decline: the entrainment of drier air at low levels from the northwest, and increasing south-southwesterly vertical shear. As Floyd neared the North Carolina coast late on the 15th, its maximum winds decreased below category three status.

After turning toward the north-northeast with forward speed increasing to near 15 knots, Hurricane Floyd made landfall near Cape Fear, North Carolina at 0630 UTC 16 September as a category two hurricane with estimated maximum winds near 90 knots. Floyd was losing its eyewall structure as it made landfall. Continuing to accelerate north-northeastward, Floyd's center passed over extreme eastern North Carolina on the morning of the 16th and over the greater Norfolk, Virginia area around 1500 UTC that day. Floyd then weakened to a tropical storm and moved swiftly along the coasts of the Delmarva peninsula and New Jersey on the afternoon and early evening of the 16th, reaching Long Island by 0000 UTC 17 September. By that time, the storm's forward speed had increased to near 29 knots. The system decelerated as it moved into New England.

By late on the 16th and early on the 17th, Floyd was becoming more involved with a frontal zone that existed along the Atlantic seaboard. The system took the form of a frontal low and thus became extratropical by the time it reached the coast of Maine at 1200 UTC 17 September. The cyclone turned toward the northeast and then east-northeast, moving over the coast of New Brunswick late on the 17th, Prince Edward Island early on the 18th and Newfoundland late on the 18th and early on the 19th. Floyd's extratropical remnant merged with a large extratropical low over the north Atlantic and was no longer a distinct entity by 1800 UTC 19 September.

b. Meteorological Statistics

Table 1 lists the best track positions and intensities at six-hourly intervals. Figure 1 is a display of this track.

Figure 2a, Figure 2b, and Figure 3 depict the best track curves of maximum one-minute average "surface" (10 meters above ground level) wind speed and minimum central sea-level pressure, respectively, as a function of time. Also plotted on Figure 2a and Figure 3 are aircraft reconnaissance and dropsonde data from the U.S. Air Force Reserves (the Hurricane Hunters) and NOAA, estimates from analyses of surface synoptic data, as well as Dvorak-technique estimates from the Tropical Analysis and Forecast Branch, TAFB, the Satellite Analysis Branch, SAB, and the U.S. Air Force Weather Agency (AFGWC in the figures) using satellite imagery. Figure 2b also shows the best track wind speed curve, but with only in situ data, i.e. flight level and dropsonde wind measurements. In both Figure 2a and Figure 2b the flight level winds are adjusted for elevation (90% of 700 mb wind speeds, 80% of 850 mb speeds, and 85% of 1500 ft speeds), and dropsonde wind measurements above the surface are adjusted to the 10 meter level using a mean hurricane eyewall profile determined by previous dropsonde measurements.

The peak intensity of Floyd, 135 knots, is based upon roughly 90% of the highest flight level (700 mb) winds of 149 knots at 0933 UTC 13 September. Minimum dropsonde-measured central pressure was 921 mb at 1121 UTC on that date.

Floyd is estimated to have been a 90-knot hurricane at landfall in North Carolina.

There was a 10 meter anemometer measurement of sustained winds of 83 knots at 0710 UTC with gusts to 106 knots at 0716 UTC taken by University of Oklahoma meteorology professor Josh Wurman near Topsail Beach North Carolina. There were also unofficial reports of peak wind gusts to 120 knots (at 8 stories elevation) at Wrightsville Beach and 104 knots at the Wilmington Emergency Operations Center.

Table 2 lists ship reports of tropical storm force or greater wind speeds associated with Floyd. Table 3 lists a selection of surface observations from land stations and data buoys. Floyd's eye passed over NOAA data buoy 41010, located about 105 n mi east-northeast of Cape Canaveral, around 0900 UTC 15 September. That buoy reported maximum 8-minute averaged winds of 72 knots at an anemometer height of 5 meters. At least three factors would imply a higher value for the 1-minute, 10 meter wind speed from the buoy observation: 1) going from an 8-minute to a 1-minute average; 2) going from 5 meters to 10 meters elevation; and 3) the presence of waves over 50 feet high. The best track intensity of Floyd when it passed over the buoy is near 100 knots, as indicated by dropsonde and aircraft flight level wind data. The center of the hurricane passed about 25 n mi west of the Frying Pan Shoals C-MAN station located about 30 n mi southeast of Cape Fear at 0500 UTC 16 September. This station reported winds sustained at 86 knots for a 20-minute period centered at that time, at an anemometer height of 44 meters.

On 13 September, just after Floyd reached maximum strength, there was evidence of a concentric eyewall. Figure 4 is a sequence of microwave images produced by the Naval Research Laboratory. Note that in the first image, during the deepening phase, there was a dominant inner eyewall with an eye diameter of 20 to 25 n mi. Later on, after peak intensity was reached, there was some indication of a concentric eyewall, particularly in the last image of this sequence. It is interesting to note that after this period, there was an apparent eyewall replacement, as suggested in the microwave image sequence shown in Figure 5, and in radar imagery from NOAA/WP-3D aircraft research missions (not shown). It can be seen that the inner eyewall was dissipating while Floyd was centered near Eleuthera. This corresponded to a weakening of the hurricane to near 105 knots. The outer convective ring became the new eyewall by the time Floyd was centered over Abaco, corresponding to an eye diameter near 50 n mi. Afterwards, the new eye failed to contract significantly, while Floyd re-strengthened just slightly as it reached Abaco. After the disintegration of the inner eyewall the large-scale environment, as noted in the previous section, became less favorable. Consequently, after leaving the Bahamas, Floyd never regained its former intensity and, in fact, slowly weakened.

Heavy rainfall preceded Floyd over the mid-Atlantic states due to a pre-existing frontal zone and the associated overrunning. Hence, even though the tropical cyclone was moving fairly quickly, precipitation amounts were very large. Rainfall totals as high as 15 to 20 inches were recorded in portions of eastern North Carolina and Virginia. At Wilmington, North Carolina, the storm total of 19.06 inches included a 24-hour record of 15.06 inches. Totals of 12 to 14 inches were observed in Maryland, Delaware, and New Jersey. New records were set in Philadelphia for the most amount of rain in a calendar day, 6.63 inches. In southeastern New York, rainfall totals were generally in the 4 to 7 inch range but there was a report of 13.70 inches at Brewster. Totals of nearly 11 inches were measured in portions of New England.

Storm surge values as high as 9 to 10 feet were reported along the North Carolina coast.

A number of tornadoes were sighted in eastern North Carolina. There was a confirmed tornado in Bertie County and another in Perquimans County. The latter tornado destroyed two houses and damaged three or four others. At least ten tornadoes were reported by spotters in the Newport/Morehead City County Warning area, and these apparently caused some structural damage. Four tornadoes or funnel clouds were seen in the Wilmington area, but no damage was apparent.

c. Casualty and Damage Statistics

There were 57 deaths that were directly attributable to Floyd, 56 in the United States and 1 in Grand Bahama Island. The death toll by state is as follows: North Carolina 35, Pennsylvania 6, New Jersey 6, Virginia 3, Delaware 2, New York 2, Connecticut 1, and Vermont 1. Most of these deaths were due to drowning in freshwater flooding. Floyd was the deadliest hurricane in the United States since Agnes of 1972.

In the United States, the Property Claims Services Division of the Insurance Services Office reports that insured losses due to Floyd totaled 1.325 billion dollars. Ordinarily this figure would be doubled to estimate the total damage. However, in comparison to most hurricane landfalls, in the case of Floyd there was an inordinately large amount of freshwater flood damage, which probably alters the two to one damage ratio. Total damage estimates range from 3 to over 6 billion dollars.

d. Forecast and Warning Critique

When averaged over the entire lifetime of the hurricane, the track forecasts for Floyd were excellent. Table 4 shows the average track errors for the official forecast and for a selection of objective guidance models. It can be seen that the average official forecast errors were substantially below the most recent ten-year averages. Also, on average, the official forecasts were better than all of the guidance except the UKMI model which had average track errors that were about equal to those of the official forecasts.

Although the overall average official forecast errors for Floyd were extremely low, the official forecasts were just ordinary if one considers only the period when hurricane warnings were in effect for the United States,. For example, the average 24-hour track forecast error for the latter period was roughly the same as the most recent ten-year average. Official track forecasts during the latter period also had a westward bias, and were somewhat slow. For example, the 36-hour official track forecasts during the period when hurricane warnings were in effect for the United States were an average of 104 n mi too far west and 70 n mi too far south. All of the track guidance models showed a similar westward and slow bias during this period.

Official intensity forecasts were fairly good (errors of 10 knots or less) for the first couple of days of Floyd's history. However, there were some large underforecasts of intensity, by as much as 30 to 40 knots, from 10-12 September. After Floyd reached its maximum intensity, the official forecasts did not show enough weakening. From 13 September onward, the wind speed was overpredicted in the advisories at practically every forecast time interval, by as much as 30 to 40 knots, and even 50 knots in one occasion. The Statistical Hurricane Intensity Prediction Scheme, SHIPS, performed similarly.

Table 5 is a chronology of the various watches and warnings that were issued for Floyd. A hurricane warning was issued for the northwest Bahamas more than 24 hours prior to the arrival of the eyewall at Eleuthera. For the United States, practically the entire east coast (the greater Miami area northward to Plymouth Massachusetts) was put under a hurricane warning for Floyd. To the authors' knowledge, the last time such an event occurred was during Hurricane Donna of 1960. Hurricane warnings for the southeast Florida coast proved unnecessary. However, given the forecast uncertainty and the required response times for evacuations and other preparations for such a large, severe hurricane, it was prudent to issue such warnings. The hurricane warning was issued for the coast of North Carolina at 0300 UTC 15 September. This is about 26-27 hours prior to the arrival of the eyewall in the Cape Fear area. Generally, for the coasts of South and North Carolina, hurricane warnings were issued at least 24 hours before the onset of tropical storm force winds.

According to preliminary information provided to the Federal Emergency Management agency, over 2 million people were evacuated for Floyd in the United States. This is probably the largest evacuation in U.S. history.


Some of the data in this report was furnished by local National Weather Service Offices in Miami, Melbourne, Jacksonville, Charleston, Wilmington, Newport/Morehead City, Raleigh/Durham, Wakefield, Baltimore/Washington, Mount Holly, New York, and Taunton. Stephen Baig produced the track chart, and James Franklin produced the wind and pressure plots.

Figure 1. Best track for Hurricane Floyd, 7-17 September 1999.

Figure 2a. Best track maximum sustained wind speed curve for Hurricane Floyd, showing all available intensity estimates and wind observations. Aircraft wind measurements have been adjusted for elevation (90% of 700 mb wind speeds, 80% of 850 mb speeds, and 85% of 1500 ft speeds), and dropsonde wind measurements above the surface are adjusted to the 10 meter level using a mean hurricane eyewall profile determined by previous dropsonde measurements. Vertical line denotes landfall.

Figure 2b. Best track maximum sustained wind speed curve for Hurricane Floyd, showing only in situ wind observations adjusted for elevation as indicated in Figure 2a.

Figure 3. Best track minimum central pressure curve and central pressure observations or estimates for Hurricane Floyd. Vertical line denotes landfall.

Figure 4. Sequence of microwave images of Hurricane Floyd at: (a) 0116 UTC, (b) 1122 UTC, (c) 1347 UTC, and (d) 2240 UTC 13 September, 1999.

Figure 5. Sequence of microwave images of Hurricane Floyd at: (a) 2240 UTC 13 September, (b) 0104 UTC, (c) 1110 UTC, and (d) 2228 UTC 14 September, 1999.

Table 1. Best track, Hurricane Floyd, 7 - 17 September, 1999
Position Pressure
Wind Speed
Lat. (°N)Lon. (°W)
7/180014.6 45.6100825tropical depression
8/000015.0 46.9100730"
060015.3 48.2100535tropical storm
120015.8 49.6100340"
180016.3 51.1100045"
9/000016.7 52.6100045"
060017.1 53.9100345"
120017.3 55.1100350"
180017.9 56.399660"
10/000018.3 57.299560"
060018.6 58.299060"
120019.3 58.898970hurricane
180020.2 59.697570"
11/000020.8 60.497180"
060021.4 61.196395"
1800 22.563.096690"
180030.679.1947 95"
16/000032.178.7950 90"
180038.075.397460tropical storm
17/060042.172.198350 tropical storm
1800 47.759.399235"
1800    merged with low
13/120023.971.4921135minimum pressure
14/120025.476.3930105Near Alice Town,
14/190026.377.1932120Near Cherokee Sound,
16/063033.878.095690Near Cape Fear,
North Carolina

Table 2. Ship reports of 34 knots or higher wind speed associated with Hurricane Floyd, September 1999.
Ship call sign Lat. (°N) Lon. (°W) Wind
12/1800DGOO23.569.5340/37 998.5
12/2100DGOO24.169.8030/43 994.8
13/0000DGOO24.569.9040/45 994.8
13/0300DGOO24.970.3040/52 997.0
13/0600DGOO25.670.5040/52 998.5
13/0900DGOO26.370.8060/52 999.5
13/1800KHRH19.574.7360/50 994.0
14/0900WGJT22.073.5180/35 998.2
16/0000WRGQ31.575.4160/46 (898.1)
16/2100DEDI40.470.9130/42 998.0
17/0000DEDI40.470.8140/50 993.3

Table 3. Hurricane Floyd, selected surface observations, September 1999.
Maximum surface wind speed
Location Press.
gust (kts)
(storm total)
Grand Bahama Island983.015/0100526514/2000 5.27 
Little Harbor Abacos929.014/1910     9.32
Nassau  5568    
Craig Field994.615/165337 15/1929   
Daytona Beach991.815/1353366015/1053  1.23
Fowey Rocks Lighthouse995.514/2300364414/1600   
Ft. Lauderdale Exec994.914/2253233315/0653  0.01
Ft. Lauderdale Int'l994.614/2253253614/2201  0.10
Ft. Pierce989.515/0735294315/0736   
Gainesville994.615/165333 15/1407   
Jacksonville Int'l995.315/165640 15/0907   
Lake Worth Pier993.414/2200324914/1700   
Melbourne Airport989.115/0900455915/0501  1.35
Melbourne WFO  325215/0655   
Miami995.814/2256192915/0322  0.04
Ocala998.015/103528 15/1535   
Orlando993.815/0853244215/0853  1.26
Patrick AFB (COF)  495715/0820   
Sanford  253714/2024  3.20
Tamiami Airport996.414/2253213114/1953   
West Palm Beach992.915/0453273814/1941  0.38
Alma999.715/`95028 15/1746   
Brooklet       0.41
Dover       0.40
Ludowici       0.52
Newington       0.85
Rocky Ford       0.20
Savannah Airport  354615/1810   
St. Simon's Island993.215/180440 15/1804   
South Carolina 
Allendale       0.67
Beaufort       1.83
Charleston City Office  507416/0150  3.99
Charleston Harbor      10.1 
Charleston Int'l Airport989.515/0052445816/0046  3.91
Edisto Beach State Park  334716/0029   
Florence Airport991.216/0655365416/0158  4.04
Folly Beach  476215/2300   
Grand Strand977.016/0553 5716/0523   
Ladson Oakbrook       4.30
Myrtle Beach Airport979.716/0553 6216/0455  16.06
Myrtle Beach Springmaid Pier   6816/0500   
Ridgeville       3.58
St. George       1.90
Walterboro       2.50
Williams       2.42
North Carolina 
Beaufort976.016/0409425816/0405  5.56
Castle Hayne 2E   8116/0715   
Castle Hayne 3SW   10416/0845   
Cherry Point MCAS961.416/0555567116/0405  3.27
Elizabeth City968.516/1418345616/1346  2.65
Federal Point   9716/0620   
Flemington   8016/0625   
Frisco983.816/0740516116/0805  0.34
Greenville   5116/0800   
Holden Beach  426416/0820   
Manteo   5316/1000   
Masonboro Island      10.3 
Mt. Olive   6516/0520   
Myrtle Grove   8916/0540   
Newport   5816/0454   
New Bern961.116/0543395816/0501  4.29
New River959.016/0426446816/0556  8.26
Oak Island  526916/0820 10.0 
Pleasure Island      10.0 
Rocky Mount/Wilson Airport       15.15
Seymour Johnson AFB983.016/0955456016/1055   
South River       3.50*
Washington   4116/0800   
Wilmington Airport959.716/0755547516/0855  19.06
Wilmington Corning Plant   8916/0700   
Wilmington EOC   10416/0845   
Wrightsville Beach   120    
Fort Eustis985.216/1455253716/1640   
Glouchester       11.25
Hampton       7.50
James City County       14.30
Langley AFB  405516/1355   
Lower James City       12.83
Newport News983.416/1558334416/1623  16.57
Norfolk Airport977.116/1551274016/1303   
Norfolk NAS979.116/1555384816/1609   
Oceana NAS975.716/155635 16/1656   
Portsmouth978.316/1600305216/1614  10.10
Richmond991.916/1640294416/1405  6.54
Smithfield       12.50
Wakefield WFO       12.73
Weems       10.83
Annapolis       11.60
Cambridge      2.5 
Chestertown       14.00
Lewisetta      3.5 
Martin State Airport989.0       
Mid-Bay Buoy   6016/1710   
Ocean City976.816/1853314516/1653  1.71
Patuxent NAS991.0 303616/1555   
Salisbury980.416/1851284216/2150  5.08
Solomon's Island      3.0 
St. Inigoes987.6       
Tall Timbers   6216/2040  11.10
Thomas Point Light  434916/1300   
Cape Henlopen   5616/PM   
Greenwood       10.58
Lewes     2.6 6.76 
Vernon       12.36
New Jersey 
American Corners       10.20
Atlantic City980.216/2054233416/23452.06.22 
Caldwell/Essex Co. Airport987.816/2353 3816/2353  10.21
Cape May     2.67.36 
Doylestown       10.07
Federalsburg       11.20
Neshanic       10.07
Newark Int'l Airport985.116/2351384616/2351  6.22
Pequannock       11.04
Sandy Hook981.016/2306344517/00241.96.57 
Somerville       13.34
Teterboro Airport985.016/2351243816/2351  8.53
Wayne/Iflows       12.21
White House       12.98
New York 
Central Park983.816/2250253616/1450  5.02
Farmingdale Airport981.616/2353233716/2053  3.13
HPN Airport985.817/0050254216/2350  6.26
Islip/MacArthur Airport983.417/0156273716/2356   
JFK Int'l Airport982.516/2351304117/0051  3.27
LaGuardia Airport983.716/2351304117/0051  4.94
MGJ Airport  294416/2039   
MTP Airport986.917/0254223717/0454   
Newburgh/Stewart Airport992.617/0045345416/2245   
NWS Upton       3.50
Westhampton Airport984.817/0153284317/0153   
White Plains Airport985.817/0050254216/2350   
Beverly   31    
Blue Hill Observatory-Milton   40    
Boston      10.7 
Boston/Logan Airport   38    
Brewster   6317/0545   
Buzzards Bay  475717/0300   
Fox Point Hurricane Barrier     4.2  
Hadley       9.60
Hyannis   62    
Lawrence   32    
Martha's Vineyard   34    
Nantucket   32  1.3 
New Bedford Hurr. Barrier   6417/06002.5  
Norwood   27    
Orange   29    
Plymouth   33    
Southwick       9.16
Taunton   38    
Westfield   37    
Worcester   30    
Rhode Island 
Block Island   39    
Newport   35  2.6 
Providence   35  5.9 
Westerly   31    
Bridgeport Airport981.817/0154293916/2254   
Bristol       10.80
Burlington       9.45
Danbury Airport987.117/0153152117/0153   
Groton/New London Airport986.817/0145304317/0045   
Hartford Airport985.417/0253      
MMK Airport986.417/0155203417/0155   
New Haven Airport983.817/014533     
Southington       9.14
Willimantic985.817/0352 31    
Windsor Locks   37    
New Hampshire 
Manchester   28    
NOAA National Data Buoy Center buoys
41004 (30.5N 79.1W)  547216/0200   
41009 (28.5N 80.2W)980.915/0900527015/1000   
41008 (31.4N 80.9W)  243115/2100   
41010 (28.9N 78.5W)939.615/0900729115/0700   
44009 (38.5N 74.7W)976.016/1900395216/1800   
44014 (36.8N 74.8W)981.416/1600506616/1615   
44025 (40.3N 73.2W)980.017/0000334317/0600   
NOAA National Data Buoy Center C-MAN stations
BUZM3 (41.4N 71.0W)  475717/0300   
CLKN7 (34.6N 76.5W)974.916/0500637916/0450   
DSLN7 (31.2N 75.3W)985.816/0730698216/0750   
DUCN7 (36.2N 75.8W)977.016/0900678316/0850   
FPSN7 (33.5N 77.6W)958.716/0600869716/0512   
SAUF1 (29.9N 81.3W)992.915/120058 15/1200   

aASOS and C-MAN are 2 min; buoys are 8 min.
bDate/time is for sustained wind when both sustained and gust are listed.
cStorm surge is water height above normal astronomical tide level.
dStorm tide is water height above National Geodetic Vertical Datum (1929 mean sea level).

Table 4. Preliminary forecast evaluation of Hurricane Floyd, heterogeneous sample. (Errors in nautical miles for tropical storm and hurricane stages with number of forecasts in parenthesis).
Forecast Technique Period (hours)
CLIP 40 (35) 88 (33)148 (31)206 (29)312 (25)
GFDI 36 (34) 71 (32) 97 (30)115 (28)153 (25)
GFDL* 31 (30) 66 (30) 96 (28)109 (26)155 (24)
LBAR 30 (34) 59 (32) 92 (30)112 (28)120 (24)
AVNI 38 (35) 77 (33)119 (31)141 (29)187 (25)
BAMD 37 (34) 70 (32)106 (30)147 (28)239 (24)
BAMM 50 (34) 96 (32)137 (30)175 (28)243 (24)
BAMS 63 (34)123 (32)173 (30)207 (28)263 (24)
A98E 35 (33) 72 (31)113 (29)120 (27)174 (24)
NGPI 39 (29) 69 (27)101 (25)123 (23)146 (19)
UKMI 29 (32) 54 (30) 66 (26) 76 (24) 97 (21)
NHC OFFICIAL 28 (35) 53 (33) 73 (31) 73 (29)104 (25)
NHC OFFICIAL 1989-1998 10-year average 48 (2005) 89 (1790)128 (1595)164 (1410)242 (1107)

* GFDL output not available until after forecast issuance.

Table 5. Watch and warning summary, Hurricane Floyd, September 1999
Action Location
09/2100Tropical storm watch issuedAntigua, Barbuda, Anguilla, and Dutch Saint Maarten
09/2200Tropical storm watch issuedFrench Saint Martin and Saint Barthelemy
11/0300Tropical storm watch discontinuedAntigua, Barbuda, Anguilla and Dutch Saint Maarten
11/0300Tropical storm watch discontinuedFrench Saint Martin and Saint Barthelemy
12/0900Tropical Storm warning and hurricane watch issuedTurks, Caicos, and Southeast Bahamas
12/0900Hurricane watch issuedCentral Bahamas
13/0000Hurricane warning issuedCentral Bahamas
13/0000Hurricane watch issuedNorthwest Bahamas
13/0900Hurricane watch upgraded to hurricane warningNorthwest Bahamas
13/0900Hurricane watch issuedFlorida: South of Flagler Beach to Hallandale
13/1500Hurricane watch extendedSouth to include Miami-Dade County and north of Flagler Beach, Florida to Brunswick, Georgia
13/1800Hurricane watch extendedIncluding Lake Okeechobee
13/2100Hurricane watch upgraded to hurricane warningFlorida City, Florida to south of Brunswick, Georgia
13/2100Tropical storm warning issuedFlorida Keys, north of Seven Mile Bridge
13/2100Hurricane watch issuedGeorgia: Brunswick to Savannah
14/0300Hurricane watch extendedNorth of Savannah, Georgia to Little River Inlet, South Carolina
14/0900Tropical storm warning discontinuedTurks and Caicos Islands
14/1500Tropical storm warning discontinuedSoutheast Bahamas
14/2100Tropical storm warning discontinuedFlorida Keys, from the Seven Mile Bridge northward
14/2100Hurricane warning extendedGeorgia and South Carolina coasts to Little River Inlet, South Carolina
14/2100Hurricane warning downgraded to tropical storm warningFlorida: Florida City to Boca Raton
14/2100Hurricane watch extendedNorth of Little River Inlet, South Carolina to Cape Charles Light, Virginia, south of New Point Comfort, including Pamlico and Albermarle sounds
15/0300Hurricane warning extendedNorth of Little River Inlet, South Carolina to the North Carolina/Virginia border
15/0300Hurricane warning discontinuedFlorida: Boca Raton to Ft. Pierce
15/0300Hurricane watch extendedNorth Carolina/Virginia border to Chincoteague, Virginia, including Chesapeake Bay, south of Smith Point
15/0300Hurricane warning discontinuedCentral Bahamas
15/0300Tropical storm warning discontinuedFlorida: Florida City to Ft. Pierce
15/0600Hurricane warning discontinuedNorthwest Bahamas: New Providence, Bimini, Andros, and Berry Islands
15/0900Tropical storm watch issuedChincoteague, Virginia to Cape Henlopen, Delaware, including Chesapeake Bay north of Smith Point and the Potomac from Cobb Island to Smith Point
15/1200Hurricane warning discontinuedFlorida: South of Sebastian Inlet to Ft. Pierce
Northwest Bahamas: Grand Bahama and Abaco Islands
15/1500Hurricane warning discontinuedFlorida: Sebastian Inlet to Titusville
15/1500Tropical storm watch extendedNorth of Chincoteague, Virginia to Sandy Hook, New Jersey, including Delaware Bay
15/1700Tropical storm watch extendedNorth of Sandy Hook, New Jersey to Montauk Point on Long Island, New York, including Delaware Bay
15/1900Hurricane warning discontinuedFlorida: Titusville to Fernandina Beach
15/2100Hurricane warning extendedNorth of North Carolina/Virginia border to Chincoteague, Virginia, including Chesapeake Bay, south of Smith Point
15/2100Tropical storm watch upgraded to tropical storm warning North of Chincoteague, Virginia to Sandy Hook, New Jersey, including northern Chesapeake Bay, the Potomac Basin, and Delaware Bay
15/2100Tropical storm watch extendedNorth of Sandy Hook, New Jersey to the Merrimack River, Massachusetts, including Long Island Sound
16/0300Hurricane warning discontinuedNorth of Fernandina Beach, Florida to Edisto Beach, South Carolina
16/0300Hurricane warning extendedNorth of Chincoteague, Virginia to Cape Henlopen, Delaware
16/0300Tropical storm warning extendedNorth of Sandy Hook, New Jersey to Plymouth, Massachusetts
16/0900Hurricane warning extendedNorth of Cape Henlopen, Delaware to Manasquan Inlet, New Jersey and from Moriches Inlet, New York to Plymouth, Massachusetts
16/0900Tropical storm warning extendedNorth of Plymouth, Massachusetts to Merrimack River, Massachusetts
16/1100Hurricane warning discontinuedFrom South Santee River, South Carolina, southward
16/1300Hurricane warning discontinuedSouth Santee River, South Carolina to Surf City, North Carolina
16/1500Hurricane warning discontinuedNorth Carolina: North of Surf City to Cape Hatteras
16/1800Hurricane warning discontinuedCape Hatteras, North Carolina to Cape Charles Light, Virginia, including southern Chesapeake Bay
16/2100Hurricane warning downgraded to tropical storm warningCape Charles Light, Virginia to the Merrimack River, Massachusetts, including Chesapeake Bay, the Potomac Basin, Delaware Bay, and Long Island Sound
17/0300Tropical storm warning discontinuedCape Charles Light, Virginia to Sandy Hook, New Jersey, including Chesapeake Bay, the Potomac Basin, and Delaware Bay
17/0900Tropical storm warning discontinuedSandy Hook, New Jersey to the Merrimack River, Massachusetts, including Long Island Sound


Last updated January 26, 2000