List of Category 5 Atlantic hurricanes

The list of Category 5 Atlantic hurricanes encompasses 32 tropical cyclones that reached Category 5 intensity on the Saffir–Simpson Hurricane Scale within the Atlantic Ocean (north of the equator), the Caribbean Sea and Gulf of Mexico. They are the most catastrophic hurricanes that can form on planet Earth. They are relatively rare in the Atlantic Ocean, and generally occur only about once every three years on average in the Atlantic basin. In general, Category 5s form in clusters in single years. Landfalls by storms at Category 5 strength are rare due to the generally northeastward path of tropical cyclones in the Northern Hemisphere's mid-latitudes. This is caused by the westerlies, which recurve strong hurricanes towards colder waters in the open Atlantic Ocean. However, the easterly large-scale surface winds in the tropics may steer strong hurricanes in the Caribbean Sea towards land areas.

Only four times—in the 1960, 1961, 2005 and 2007 hurricane seasons—have multiple Category 5 hurricanes formed. Only in 2005 have more than two Category 5 storms formed, and only in 2007 has more than one made landfall at Category 5 strength.[1]

Contents

Statistics

Saffir–Simpson Hurricane Scale
TD TS C1 C2 C3 C4 C5

A Category 5 hurricane has sustained winds greater than 135 knots (155.4 mph; 250.0 km/h). "Sustained winds" refers to the average wind speed observed over one minute at 10 metres (32 ft 9.7 in) above ground, which is the standard height windspeed is measured at to avoid interference by obstacles and obstructions. Brief gusts in hurricanes are typically up to 50 percent higher than sustained winds.[2] Because a hurricane is (usually) a moving system, the wind field is asymmetric, with the strongest winds on the right side (in the Northern Hemisphere), relative to the direction of motion. The highest winds given in advisories are those from the right side.[3]

Between 1924 and 2007, 32 hurricanes were recorded at Category 5 strength. No Category 5 hurricanes were observed officially before 1924. It can be presumed that earlier storms reached Category 5 strength over open waters, but the strongest winds were not measured. The anemometer, a device A reanalysis of weather data is ongoing by researchers who may upgrade or downgrade other Atlantic hurricanes currently listed at Categories 4 and 5.[4] For example, the 1825 Santa Ana hurricane is suspected to have reached Category 5 strength.[5] Furthermore, paleotempestological research aims to identify past major hurricanes by comparing sedimentary evidence of recent and past hurricane strikes. For example, a “giant hurricane” significantly more powerful than Hurricane Hattie (Category 5) has been identified in Belizean sediment, having struck the region sometime before 1500.[6]

Officially, the decade with the most Category 5 hurricanes is 2000–2009, with eight Category 5 hurricanes having occurred: Isabel (2003), Ivan (2004), Emily (2005), Katrina (2005), Rita (2005), Wilma (2005), Dean (2007), and Felix (2007). The previous decade with the most Category 5 hurricanes was the 1960s, with six occurring between 1960 and 1969. (Ethel, Donna, Carla, Hattie, Beulah, and Camille).[1]

Six Atlantic hurricanes—Allen, Andrew, Isabel, Ivan, Dean and Felix—have reached Category 5 intensity on more than one occasion; that is, by reaching Category 5 intensity, weakening to a Category 4 or lower, and then becoming a Category 5 again. Such hurricanes have their dates shown together. However, no Atlantic hurricane has reached Category 5 intensity more than three times, as Allen, Isabel and Ivan each reached that intensity on three separate occasions. Andrew, Dean and Felix are the only other storms to have reached Category 5 on multiple occasions, each doing it twice. Hurricane Allen holds the record for most overall time spent as a Category 5, while Hurricanes Dog and Ivan hold the record for most time spent consecutively as a Category 5.[1][7]

The minimum pressure of the more recent systems was measured by recon aircraft using dropsondes, or by determining it from satellite imagery using the Dvorak technique. For older storms, pressures are often incomplete. The only readings came from ship reports, land observations, or aircraft reconnaissance. None of these methods can provide constant pressure measurements. Thus, sometimes the only measurement can be from when the hurricane was not a Category 5. Consequently, the lowest measurement is sometimes unrealistically high for a Category 5 hurricane.

These pressure values do not match up with the wind readings. This happens because the wind speed of a hurricane depends on both its size and how rapidly the pressure drops as the hurricane's center approaches. Thus, a hurricane in an environment of high ambient pressure will have stronger winds than a hurricane in an environment of low ambient pressure, even if they have identical central pressures.[8]

Category 5 Atlantic hurricanes

Storm
name
Season Dates as a
Category 5
Time as a
Category 5
Peak one-minute
sustained winds
Pressure
(hPa & inHg)
"Cuba" 01924-10-19 October 19, 1924 1924 October 19 &10000000000000012000000 12 hours 165 mph (270 km/h) &10000000000000910000000910 hPa (27 inHg)
San Felipe II-"Okeechobee" 01928-09-13 September 13, 1928 1928 September 13–14 &10000000000000012000000 12 hours 160 mph (260 km/h) &10000000000000929000000929 hPa (27.4 inHg)
"Bahamas" 01932-09-05 September 5, 1932 1932 September 5–6 &10000000000000024000000 24 hours 160 mph (260 km/h) &10000000000000931000000931 hPa (27.5 inHg)
"Labor Day" 01935-09-03 September 3, 1935 1935 September 3 &10000000000000006000000 6 hours 185 mph (295 km/h) &10000000000000892000000892 hPa (26.3 inHg)
"New England" 01938-09-19 September 19, 1938 1938 September 19–20 &10000000000000018000000 18 hours 160 mph (260 km/h) &10000000000000938000000938 hPa (27.7 inHg)
"Fort Lauderdale" 01947-09-16 September 16, 1947 1947 September 16–17 &10000000000000030000000 30 hours 160 mph (260 km/h) &10000000000000929000000929 hPa (27.4 inHg)
Dog 01950-09-05 September 5, 1950 1950 September 5–7 &10000000000000060000000 60 hours 185 mph (295 km/h) &10000000000000948000000948 hPa (28.0 inHg)
Easy 01951-09-07 September 7, 1951 1951 September 7–8 &10000000000000018000000 18 hours 160 mph (260 km/h) &10000000000000957000000957 hPa (28.3 inHg)
Janet 01955-09-27 September 27, 1955 1955 September 27–28 &10000000000000018000000 18 hours 175 mph (280 km/h) &10000000000000914000000914 hPa (27.0 inHg)
Cleo 01958-08-16 August 16, 1958 1958 August 16 &10000000000000006000000 6 hours 160 mph (260 km/h) &10000000000000948000000948 hPa (28.0 inHg)
Donna 01960-09-04 September 4, 1960 1960 September 4 &10000000000000012000000 12 hours 160 mph (260 km/h) &10000000000000932000000932 hPa (27.5 inHg)
Ethel 01960-09-15 September 15, 1960 1960 September 15 &10000000000000006000000 6 hours 160 mph (260 km/h) &10000000000000972000000972 hPa (28.7 inHg)
Carla 01961-09-11 September 11, 1961 1961 September 11 &10000000000000018000000 18 hours 175 mph (280 km/h) &10000000000000932000000932 hPa (27.5 inHg)
Hattie 01961-10-30 October 30, 1961 1961 October 30–31 &10000000000000018000000 18 hours 160 mph (260 km/h) &10000000000000920000000920 hPa (27 inHg)
Beulah 01967-09-20 September 20, 1967 1967 September 20 &10000000000000018000000 18 hours 160 mph (260 km/h) &10000000000000923000000923 hPa (27.3 inHg)
Camille 01969-08-17 August 17, 1969 1969 August 17–18 &10000000000000018000000 18 hours 190 mph (305 km/h) &10000000000000905000000905 hPa (26.7 inHg)
Edith 01971-09-09 September 9, 1971 1971 September 9 &10000000000000006000000 6 hours 160 mph (260 km/h) &10000000000000943000000943 hPa (27.8 inHg)
Anita 01977-09-02 September 2, 1977 1977 September 2 &10000000000000012000000 12 hours 175 mph (280 km/h) &10000000000000926000000926 hPa (27.3 inHg)
David 01979-08-30 August 30, 1979 1979 August 30–31 &10000000000000042000000 42 hours 175 mph (280 km/h) &10000000000000924000000924 hPa (27.3 inHg)
Allen 01980-08-05 August 5, 1980 1980 August 5–9† &10000000000000072000000 72 hours 190 mph (305 km/h) &10000000000000899000000899 hPa (26.5 inHg)
Gilbert 01988-09-13 September 13, 1988 1988 September 13–14 &10000000000000024000000 24 hours 185 mph (295 km/h) &10000000000000888000000888 hPa (26.2 inHg)
Hugo 01989-09-15 September 15, 1989 1989 September 15 &10000000000000006000000 6 hours 160 mph (260 km/h) &10000000000000918000000918 hPa (27.1 inHg)
Andrew 01992-08-23 August 23, 1992 1992 August 23–24† &10000000000000016000000 16 hours 175 mph (280 km/h) &10000000000000922000000922 hPa (27.2 inHg)
Mitch 01998-10-26 October 26, 1998 1998 October 26–28 &10000000000000042000000 42 hours 180 mph (285 km/h) &10000000000000905000000905 hPa (26.7 inHg)
Isabel 02003-09-11 September 11, 2003 2003 September 11–14† &10000000000000042000000 42 hours 165 mph (270 km/h) &10000000000000915000000915 hPa (27.0 inHg)
Ivan 02004-09-09 September 9, 2004 2004 September 9–14† &10000000000000060000000 60 hours 165 mph (270 km/h) &10000000000000910000000910 hPa (27 inHg)
Emily 02005-07-16 July 16, 2005 2005 July 16 &10000000000000006000000 6 hours 160 mph (260 km/h) &10000000000000929000000929 hPa (27.4 inHg)
Katrina 02005-09-28 September 28, 2005 2005 August 28–29 &10000000000000018000000 18 hours 175 mph (280 km/h) &10000000000000902000000902 hPa (26.6 inHg)
Rita 02005-09-21 September 21, 2005 2005 September 21–22 &10000000000000024000000 24 hours 180 mph (285 km/h) &10000000000000895000000895 hPa (26.4 inHg)
Wilma 02005-10-19 October 19, 2005 2005 October 19 &10000000000000018000000 18 hours 185 mph (295 km/h) &10000000000000882000000882 hPa (26.0 inHg)
Dean 02007-08-18 August 18, 2007 2007 August 18–21† &10000000000000024000000 24 hours 175 mph (280 km/h) &10000000000000905000000905 hPa (26.7 inHg)
Felix 02007-09-03 September 3, 2007 2007 September 3–4† &10000000000000024000000 24 hours 175 mph (280 km/h) &10000000000000929000000929 hPa (27.4 inHg)
Reference=[1] †= Attained Category 5 status more than once

Climatology

Thirty-two Category 5s have been recorded in the Atlantic basin since 1851, when records began. Only one Category 5 has been recorded in July, seven in August, twenty in September, and four in October. There have been no officially recorded June, November or off-season Category 5 hurricanes.[1]

The July and August Category 5s reached their high intensities in both the Gulf of Mexico and the Caribbean Sea. These are the areas most favorable for tropical cyclone development in those months.[1][9]

September sees the most Category 5 hurricanes. This coincides with the climatological peak of the Atlantic hurricane season, which occurs in early September.[10] September Category 5s reached their strengths in any of the Gulf of Mexico, Caribbean Sea, and open Atlantic. These places are where September tropical cyclones are likely to form.[9] Many of these hurricanes are either Cape Verde-type storms, which develop their strength by having a great deal of open water; or so-called Bahama busters, which intensify over the warm Loop Current in the Gulf of Mexico.[11]

All four October Category 5s reached their intensities in the western Caribbean, a region that Atlantic hurricanes strongly gravitate toward late in the season.[9] This is due to the climatology of the area, which sometimes has a high-altitude anticyclone that promotes rapid intensification late in the season, as well as warm waters. Originally, there were only three Category 5s discovered in October, but reanalysis found out that a Hurricane in 1924 also reached that intensity during the month, so four Category 5s developed in October.[1]

Landfalls

All Atlantic Category 5 hurricanes except Dog, Easy, and Cleo have made landfall at some location at some strength. Most Category 5 hurricanes in the Atlantic make landfall because of their proximity to land in the Caribbean and Gulf of Mexico, where the usual synoptic weather patterns carry them towards land, as opposed to the westward, oceanic mean track of Eastern Pacific hurricanes.[12] Thirteen of the storms made landfall while at Category 5 intensity;[1] 2007 is the only year in which two storms made landfall at this intensity.[1]

Many of these systems made landfall shortly after weakening from a Category 5. This weakening can be caused by dry air near land, shallower waters due to shelving, interaction with land, or cooler waters near shore.[13] In southern Florida, the return period for a Category 5 hurricane is roughly once every 50 years.[14]

The hurricanes are listed in chronological order with their landfalls indicated. Because they never made landfall, Hurricanes Dog, Easy, and Cleo are not included. Hurricane Dog is the only Category 5 hurricane that didn't make landfalls but still caused deaths and damages.

The following table is based on the intensity at landfall, separated by category on the Saffir–Simpson Hurricane Scale.

Name Year Category 5 Category 4 Category 3 Category 2 Category 1 Tropical Storm
"Cuba" 1924 Cuba Florida Bahamas
"Okeechobee" 1928 Puerto Rico Bahamas & Florida
"Bahamas" 1932 The Bahamas
"Labor Day" 1935 Florida Keys Northwest Florida The Bahamas
"New England" 1938 New York & Connecticut
"Fort Lauderdale" 1947 The Bahamas Florida Louisiana
Janet 1955 Yucatán Peninsula Mainland Mexico
Donna 1960 Bahamas & Florida North Carolina, New York & Connecticut
Ethel 1960 Mississippi
Carla 1961 Texas
Hattie 1961 Belize Mexico
Beulah 1967 Texas Yucatán Peninsula
Camille 1969 Mississippi Cuba
Edith 1971 Nicaragua Louisiana Belize & Mexico
Anita 1977 Mexico
David 1979 Dominican Republic Dominica Florida Cuba, Bahamas & Georgia
Allen 1980 Texas
Gilbert 1988 Mexico Jamaica Mexico
Hugo 1989 Guadeloupe, Saint Croix,
and South Carolina
Puerto Rico
Andrew 1992 Eleuthera and Florida Berry Islands Louisiana
Mitch 1998 Honduras Mexico & Florida
Isabel 2003 North Carolina
Ivan 2004 Florida Grenada & Alabama
Emily 2005 Mexico (twice) Mexico Grenada
Katrina 2005 Louisiana & Mississippi Florida
Rita 2005 Louisiana
Wilma 2005 Mexico (twice) Florida
Dean 2007 Yucatán Peninsula Veracruz
Felix 2007 Nicaragua Grenada

See also

Tropical cyclones portal
Weather portal

References

  1. ^ a b c d e f g h i Hurricane Research Division (August 2011). "Atlantic hurricane best track (Hurdat)". National Oceanic and Atmospheric Administration. http://www.aoml.noaa.gov/hrd/hurdat/tracks1851to2010_atl_reanal.html. Retrieved 2011-09-19. 
  2. ^ Landsea, Christopher W. "Tropical Cyclone FAQ Subject: D4) What does "maximum sustained wind" mean? How does it relate to gusts in tropical cyclones?". Atlantic Oceanographic and Meteorological Laboratory. National Oceanic and Atmospheric Administration. http://www.aoml.noaa.gov/hrd/tcfaq/D4.html. Retrieved 2006-03-16. 
  3. ^ Landsea, Christopher W. "Tropical Cyclone FAQ Subject: D6) Why are the strongest winds in a hurricane typically on the right side of the storm?". Atlantic Oceanographic and Meteorological Laboratory. National Oceanic and Atmospheric Administration. http://www.aoml.noaa.gov/hrd/tcfaq/D6.html. Retrieved 2006-03-16. 
  4. ^ Staff writer (2010-06-08). "Re-analysis Project". Hurricane Research Division — Atlantic Oceanographic and Meteorological Project. National Oceanic and Atmospheric Administration. http://www.aoml.noaa.gov/hrd/data_sub/re_anal.html. Retrieved 2010-11-30. 
  5. ^ Donnelly, J. P. (2005). "Evidence of Past Intense Tropical Cyclones from Backbarrier Salt Pond Sediments: A Case Study from Isla de Culebrita, Puerto Rico, USA". Journal of Coastal Research SI42: 201–210. ISSN 0749-0208. http://www.whoi.edu/science/GG/coastal/publications/pdfs/Donnelly%20JCR%202005-Hurricane.pdf. Retrieved 2010-11-26. 
  6. ^ Mccloskey, T; G Keller (2009). "5000 year sedimentary record of hurricane strikes on the central coast of Belize". Quaternary International 195 (1-2): 53–68. Bibcode 2009QuInt.195...53M. doi:10.1016/j.quaint.2008.03.003. ISSN 1040-6182. http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VGS-4S26655-2&_user=10&_coverDate=02%2F15%2F2009&_rdoc=1&_fmt=high&_orig=search&_origin=search&_sort=d&_docanchor=&view=c&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=55065b6c2ebfb6da1b465118b6b51638&searchtype=a. Retrieved 2010-11-25. 
  7. ^ Rappaport, Edward N.. "Addendum Hurricane Andrew". National Hurricane Center. National Oceanic and Atmospheric Administration. http://www.nhc.noaa.gov/1992andrew_add.html. 
  8. ^ Landsea, Christopher W.. "Tropical Cyclone FAQ Subject: D9) What causes each hurricane to have a different maximum wind speed for a given minimum sea-level pressure?". Atlantic Oceanographic and Meteorological Laboratory. National Oceanic and Atmospheric Administration. http://www.aoml.noaa.gov/hrd/tcfaq/D9.html. Retrieved 2006-03-16. 
  9. ^ a b c Staff writer (2010). "Tropical Cyclone Climatology". National Hurricane Center. National Oceanic and Atmospheric Administration. http://www.nhc.noaa.gov/pastprofile.shtml. Retrieved 2010-11-30. 
  10. ^ Dorst, Neal (2010-06-10). "Tropical Cyclone FAQ G1) When is hurricane season ?". National Hurricane Center. National Oceanic and Atmospheric Administration. http://www.aoml.noaa.gov/hrd/tcfaq/G1.html. Retrieved 2010-11-30. 
  11. ^ Landsea, Christopher W. (2010-06-08). "Tropical Cyclone FAQ A2) What is a "Cape Verde" hurricane?". Hurricane Research Division — Atlantic Oceanographic and Meteorological Laboratory. National Oceanic and Atmospheric Administration. http://www.aoml.noaa.gov/hrd/tcfaq/A2.html. Retrieved 2010-11-30. 
  12. ^ Landsea, Christopher W (2010-06-08). "Tropical Cyclone FAQ G8) Why do hurricanes hit the East coast of the U.S., but never the West coast?". Atlantic Oceanographic and Meteorological Laboratory. National Oceanic and Atmospheric Administration. http://www.aoml.noaa.gov/hrd/tcfaq/G8.html. Retrieved 2010-11-30. 
  13. ^ Knabb, Richard D.; Rhome, Jamie R. Brown, Daniel P. (2005-12-20). "Tropical Cyclone Report Hurricane Katrina". National Hurricane Center. National Oceanic and Atmospheric Administration. p. 4. http://www.nhc.noaa.gov/pdf/TCR-AL122005_Katrina.pdf. Retrieved 30 November 2010. 
  14. ^ Landsea, Christopher W.; Franklin, James L. McAdie, Colin J. Beven, John L. Gross, James M. Jarvinen, Brian R. Pasch, Richard J. Rappaport, Edward N. Dunion, Jason P. Dodge Peter P. (2004). "A Reanalysis of Hurricane Andrew's Intensity". Bulletin of the American Meteorological Society 85 (11): 1699. Bibcode 2004BAMS...85.1699L. doi:10.1175/BAMS-85-11-1699. ISSN 0003-0007. http://www.nhc.noaa.gov/pdf/04landsea.pdf. Retrieved 2010-11-30. 

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