Atlantic hurricane
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Atlantic hurricane refers to a tropical cyclone that forms in the Atlantic Ocean north of the equator, usually in the Northern Hemisphere summer or autumn, with one-minute maximum sustained winds of 74 mph/64 kts/33 m/s. [1]
When applied to hurricanes, "Atlantic" generally refers to the entire "Atlantic basin," which includes the North Atlantic Ocean, Caribbean Sea and the Gulf of Mexico.
Most Atlantic tropical storms and hurricanes form between June 1 and November 30. The United States National Hurricane Center monitors the basin and issues reports, watches and warnings about tropical weather systems for the Atlantic Basin as one of the Regional Specialized Meteorological Centers for tropical cyclones as defined by the World Meteorological Organization.
On average, 10.1 named storms -- tropical disturbances that reach tropical storm intensity are named -- occur each season, with an average of 5.9 becoming hurricanes and 2.5 becoming major hurricanes (Category 3 or greater). The climatological peak of activity is around September 10 each season.
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[edit] Steering factors
Tropical cyclones are steered by the surrounding flow throughout the depth of the troposphere (the atmosphere from the surface to about eight miles (12 km) high. Neil Frank, former director of the United States National Hurricane Center, used the analogies such as "a leaf carried along in a stream" or a "brick moving through a river of air" to describe the way atmospheric flow affects the path of a hurricane across the ocean. Specifically, air flow around high pressure systems and toward low pressure areas influence hurricane tracks.
In the tropical latitudes, tropical storms and hurricanes generally move westward with a slight tend toward the north, under the influence of a high pressure system, the subtropical ridge that usually extends east-west across the subtropics. South of the subtropical ridge, surface easterly winds (blowing from east to west) prevail. If the subtropical ridge is weakened by an upper trough, a tropical cyclone may turn poleward and then recurve, or curve back toward the northeast into the main belt of the Westerlies. Poleward (north) of the subtropical ridge, westerly winds prevail and generally steer tropical cyclones that reach northern latitudes toward the east. The westerlies also steer nontropical cyclones with their cold and warm fronts from west to east. [2]
[edit] Climatology
Month | Total | Average |
---|---|---|
January–April | 4 | 0.1 |
May | 8 | 0.1 |
June | 35 | 0.6 |
July | 58 | 0.9 |
August | 173 | 2.8 |
September | 224 | 3.6 |
October | 114 | 1.8 |
November | 33 | 0.5 |
December | 7 | 0.1 |
Source: NOAA + additions for 2001-05 |
Climatology can be unreliable for as a sole use for a forecast, but it does serve to characterize the general properties of an average season and can be used as one of many other tools for making forecasts.
Most storms form in warm waters several hundred miles north of the equator near the Intertropical convergence zone from tropical waves. The Coriolis force is usually too weak to initiate sufficient rotation near the equator. Storms most often form in the warm waters of the Gulf of Mexico, the Caribbean Sea, and the tropical Atlantic Ocean as far east as the Cape Verde Islands, the origin of strong and long-lasting Cape Verde-type hurricanes. Systems may also strengthen over the Gulf Stream off the coast of the eastern United States.
When a tropical system forms, it usually travels west and slightly north while strengthening. After being approached by an upper trough moving west to east, and its accompanying surface cold front, many storms typically recurve to the northeast, following the trough. Recurvature typically happens near the latitude band of the Florida peninsula (25°N to 30°N). The storm weakens as it encounters cooler water, land, or vertical wind shear, sometimes transitioning into an extratropical storm.
Although most storms are found within tropical latitudes, occasionally storms will form further north and east from disturbances other than tropical waves such as cold fronts and upper-level lows.
There is a strong correlation between Atlantic hurricane activity in the tropics and the presence of an El Niño or La Niña in the Pacific Ocean. El Niño events increase the wind shear over the Atlantic, producing a less-favorable environment for formation and decreasing tropical activity in the Atlantic basin. Conversely, La Niña causes an increase in activity due to a decrease in wind shear. [3]
[edit] June
The beginning of the hurricane season is most closely related to the timing of increases in sea surface temperatures, convective instability, and other thermodynamical factors. [4] Although this month marks the beginning of the hurricane season, the month of June generally still sees little activity, with an average of about 3 tropical cyclones per 5 years.
Any tropical systems usually form in the Gulf of Mexico or off the east coast of the United States.
[edit] July
July still has relatively little activity, with about one tropical cyclone every other year. Climatologically speaking, half of seasons have their first tropical storm by July 11 with a second by August 8, using data from 1944 to 1996.
Formation usually occurs in the eastern Caribbean Sea around the Lesser Antilles, in the north and east parts of the Gulf of Mexico, in the northern Bahamas, and off the coast of The Carolinas and Virginia. Storms travel west through the Caribbean and then either move more northerly and curving near the eastern coast of the United States or southerly and entering the Gulf of Mexico.
[edit] August
Activity increases significantly in August due to lower values of wind shear than in June or July [5], with an average of about 2.8 storms per year. About half of seasons have four named systems and one hurricane total by August 30. The average season also sees one major hurricane by September 4.
[edit] September
The peak of the hurricane season in September corresponds to a time low wind shear [5] and the warmest sea surface temperatures[6]. The month of September sees an average of 3.6 storms a year. By September 24, the average season sees 7 named systems, of which 4 are hurricanes. In addition, two major hurricanes would be seen by September 28.
[edit] October
The favorable conditions found during September begin to decay in October. The main reason for the decrease in activity is increasing wind shear, although sea surface temperatures are also usually cooler than in September. [4] Activity falls off markedly, with 1.8 cyclones developing on average, though there is a climatological secondary peak around October 20.[7]. By October 21, the average season is expected to have 9 named storms with 5 hurricanes. A third major hurricane would be expected sometime between September 28 and the end of the year for half of all seasons.
In contrast to mid-season activity, in October the mean locus of formation shifts westward to the Caribbean and Gulf of Mexico, a reverse trend to the eastward progression of June through August.
[edit] November
Wind shear from westerlies increases substantially through November, generally preventing cyclone formation. [4] On average, one storm forms during November every other year. On extremely rare occasions, a major hurricane might form, such as 155 mph category four Hurricane Lenny in 1999, which formed in mid November, and Kate, a category three which formed in late November.
[edit] December to May
- Further information: Off-season storms
Few tropical cyclones can be found in the time between seasons, though about one-third of the years between 1944 and 2005 experienced an off-season tropical or subtropical cyclone. In the 61 seasons between 1944 and 2005, 8 tropical cyclones have formed in May, 7 in December, and 4 total for all four months between January and April. High vertical wind shear and low sea surface temperatures generally preclude formation. Though a tropical cyclone has been observed in the Atlantic basin in every month in the year, no tropical cyclone is officially documented to have initially formed in January. A subtropical cyclone formed in January in the 1978 season, and both Hurricane Alice and Tropical Storm Zeta formed in December and lasted into January.
[edit] Extremes
- See also: List of notable Atlantic hurricanes
- The season in which the most tropical storms formed on record was the 2005 Atlantic hurricane season (28). That season was also the one in which the most hurricanes formed on record (15).
- The 1950 Atlantic hurricane season had the most major hurricanes on record (8).
- The least active season on record since 1944 (when the database is considered more reliable) was the 1983 Atlantic hurricane season, with one tropical storm, two hurricanes, and one major hurricane. Overall, the 1914 Atlantic hurricane season remains the least active, with only one documented storm.
- The most intense hurricane on record to form in the North Atlantic basin was Hurricane Wilma (2005) (882 mbar).
- The longest-lasting hurricane was the San Ciriaco Hurricane of 1899 (28 days).
- The fastest-moving hurricane was Hurricane Emily (1987) at 69 mph.
- The most tornadoes spawned by a hurricane was 123 by Hurricane Frances (2004 season).
- The strongest landfalling hurricane was the Labor Day Hurricane of 1935 (892 mbar).
- The deadliest hurricane was the Great Hurricane of 1780 (22,000 fatalities).
- The most damaging hurricane (adjusted for inflation) was Hurricane Katrina of the 2005 season which caused $81.2 billion in damages (2005 USD).
[edit] See also
- Tropical cyclone
- Category:Atlantic hurricanes
- Category:Atlantic hurricane seasons
- List of notable Atlantic hurricanes
- List of Atlantic hurricane seasons
- South Atlantic tropical cyclone
- Atlantic Hurricane Names
- Mediterranean tropical cyclone
- Pacific hurricane
[edit] References
- ^ National Hurricane Center. Glossary of NHC/TPC Terms. Retrieved on 2006-10-28.
- ^ Hurricane Research Division. Frequently Asked Questions: Subject G6) What determines the movement of tropical cyclones? Retrieved on 2006-10-28.
- ^ Marc C. Cove, James J. O'Brien, et. al. Effect of El Niño on U.S. Landfalling Hurricanes, Revisited. Retrieved on 2006-10-28.
- ^ a b c William M. Gray and Philip J. Klotzbach. SUMMARY OF 2005 ATLANTIC TROPICAL CYCLONE ACTIVITY AND VERIFICATION OF AUTHOR’S SEASONAL AND MONTHLY FORECASTS. Retrieved on 2006-10-28.
- ^ a b Anantha R. Aiyyer. Climatology of Vertical Wind Shear Over the Tropical Atlantic. Retrieved on 2006-10-28.
- ^ Chris Landsea. Frequently Asked Questions: G5) Why do tropical cyclones occur primarily in the summer and autumn? Retrieved on 2006-10-28.
- ^ NOAA. Graph showing average activity during the hurricane Season. Retrieved on 2006-10-28.