This article is about weather phenomena. For other uses, see Hurricane (disambiguation), Typhoon (disambiguation) and Tropical storm (disambiguation).

In meteorology, a tropical cyclone (or tropical storm, typhoon or hurricane, depending on strength and location) is a type of low-pressure system which generally forms in the tropics. While some, particularly those that make landfall in populated areas, are regarded as highly destructive, tropical cyclones are an important part of the atmospheric circulation system, which moves heat from the equatorial region toward the higher latitudes.

Contents

1 A heat engine 2 Classification and terminology 3 Location 3.1 Major basins 3.2 Unusual formation areas 3.3 Timing 4 Structure 5 Formation and development 6 Dissipation 6.1 Attempts to dissipate cyclones 7 Observations 8 Effects 8.1 Beneficial effects of tropical cyclones 9 Notable cyclones 10 Naming of tropical cyclones 10.1 History of tropical cyclone naming 10.2 The naming process 11 Etymology 12 See also 13 External links

A heat engine

Structurally, a tropical cyclone is a large, rotating area of clouds, wind, and thunderstorm activity. The primary energy source of a tropical cyclone is the release of heat of condensation from water vapor condensing at high altitudes. Because of this, a tropical cyclone can be thought of as a giant vertical heat engine.

The ingredients for a tropical cyclone include a pre-existing weather disturbance, warm tropical oceans, moisture, and relatively light winds aloft. If the right conditions persist long enough, they can combine to produce the violent winds, incredible waves, torrential rains, and floods associated with this phenomenon.

This use of condensation as a driving force is the primary difference setting tropical cyclones apart from other meteorological phenomena, such as mid-latitude cyclones, which draw energy mostly from pre-existing temperature gradients in the atmosphere. To drive its heat engine, a tropical cyclone must stay over warm water, which provides the atmospheric moisture needed. The evaporation of this moisture is driven by the high winds and reduced atmospheric pressure present in the storm, resulting in a sustaining cycle.

Classification and terminology

Tropical cyclones are classified into three main groups: tropical depressions, tropical storms, and a third group whose name depends on the region.

A tropical depression is an organized system of clouds and thunderstorms with a defined surface circulation and maximum sustained winds of less than 17 metres per second (33 knots, 38 mph, or 62 km/h). It has no eye, and does not typically have the spiral shape of more powerful storms.

A tropical storm is an organized system of strong thunderstorms with a defined surface circulation and maximum sustained winds between 17 and 33 meters per second (34 to 63 knots, 39 to 73 mph, or 62 to 117 km/h). At this point, the distinctive cyclonic shape starts to develop, though an eye is usually not present.

The term used to describe tropical cyclones with maximum sustained winds exceeding 33 meters per second (63 knots, 73 mph, or 117 km/h) varies depending on region of origin, as follows:

• hurricane in the North Atlantic Ocean, North Pacific Ocean east of the dateline, and the South Pacific Ocean east of 160°E
• typhoon in the Northwest Pacific Ocean west of the dateline
• severe tropical cyclone in the Southwest Pacific Ocean west of 160°E or Southeast Indian Ocean east of 90°E
• severe cyclonic storm in the North Indian Ocean
• tropical cyclone in the Southwest Indian Ocean

This is the intensity at which tropical cyclones tend to develop an eye, which is an area of relative calm surrounded by the strongest winds of the storm, in the eyewall. The strongest of these storms have had maximum sustained windspeeds recorded at 85 meters per second (165 knot, 190 mph, 305 km/h).

In other places in the world, hurricanes have been called Bagyo in the Philippines, Chubasco in Mexico, and Taino in Haiti.

Hurricanes are categorized on a 1-to-5 scale according to the strength of their winds, using the Saffir-Simpson Hurricane Scale. A Category 1 storm has the lowest wind speeds, while a Category 5 hurricane has the strongest. These are relative terms, because lower category storms can sometimes inflict greater damage than higher category storms, depending on where they strike and the particular hazards they bring. In fact, tropical storms can also produce significant damage and loss of life, mainly due to flooding.

The U.S. National Hurricane Center classifies hurricanes of Category 3 or above as Major Hurricanes. The Joint Typhoon Warning Center classifies typhoons with wind speeds of at least 150 mi/h (67 m/s or 241 km/h; a strong Category 4 storm) as Super Typhoons.

The definition of sustained winds recommended by the World Meteorological Organization (WMO) is that of a ten-minute average, and that definition is adopted by most countries. However, a few countries use different definitions: the United States, for example, defines sustained winds based on a 1-minute average wind measured at about 10 meters (33 ft) above the surface.

An extratropical cyclone is a storm that was once tropical in nature. However, once it passed over land or cool waters, its energy source changed from released heat from condensing water to the difference in temperature between air masses. From space, these storms resemble a comma. Extratropical cyclones still can be dangerous because their continuing low pressure causes powerful winds.

In the United Kingdom and Europe, some severe northeast Atlantic cyclonic depressions are referred to as "hurricanes," even though they rarely originate in the tropics. These European windstorms can generate hurricane-force windspeeds but are not given individual names. In British shipping forecasts, winds of force 12 on the Beaufort scale are described as "hurricane force".

There is also a polar counterpart to the tropical cyclone, called an arctic cyclone.

Location

Nearly all tropical cyclones form within 30 degrees of the equator and 87% form within 20 degrees of it. Since the Coriolis effect initiates and maintains tropical cyclone rotation, such cyclones almost never form or move within about 10 degrees of the equator [1] http://www.bom.gov.au/bmrc/pubs/tcguide/ch1/figures_ch1/figure1.9.htm (where the Coriolis effect is weakest). However, it is possible for tropical cyclones to form within this boundary if another source of initial rotation is provided. These conditions are extremely rare and such storms are believed to form at a rate of less than one a century.

Most tropical cyclones form in a worldwide band of thunderstorm activity known as the Intertropical convergence zone (ITCZ).

Worldwide, an average of 80 tropical cyclones form each year.

Major basins

There are seven main basins of tropical cyclone formation:

• Western North Pacific Ocean: Tropical storm activity in this region frequently affects China, Japan, the Philippines, and Taiwan. This is by far the most active basin, accounting for one third of all tropical cyclone activity in the world. National meteorology organizations, as well as the Joint Typhoon Warning Center (JTWC) are responsible for issuing forecasts and warnings in this basin.
• Eastern North Pacific Ocean: This is the second most active basin in the world, and is also the most dense (a large number of storms for a small area of ocean). Storms which form in this basin can affect western Mexico, Hawaii and on extremely rare occasions, California. The Central Pacific Hurricane Center is responsible for forecasting the western part of this area, and the National Hurricane Center for the eastern part.
• South Western Pacific Ocean: Tropical activity in this region largely affects Australia and Oceania, and is forecast by Australia and New Guinea.
• Northern Indian Ocean: This basin is actually divided into two areas, the Bay of Bengal and the Arabian Sea, with the Bay of Bengal dominating (5 to 6 times more activity). Hurricanes which form in this basin have historically cost the most lives — most notably, the Bhola Cyclone of 1970 killed 200,000. Nations affected by this basin include India, Bangladesh, Sri Lanka, Thailand, Burma, and Pakistan, and all of these countries issue region forecasts and warnings. Rarely, a tropical cyclone formed in this basin will affect the Arabian Peninsula.
• Southeastern Indian Ocean: Tropical activity in this region affects Australia and Indonesia, and is forecast by those nations.
• Southwestern Indian Ocean: This basin is the least understood, due to a lack of historical data. Cyclones forming here impact Madagascar, Mozambique, Mauritius, and Kenya, and these nations issue forecasts and warnings for the basin.
• North Atlantic Basin: The most well studied of all tropical basins, the North Atlantic includes the Atlantic Ocean, the Caribbean Sea, and the Gulf of Mexico. Tropical cyclone formation here varies widely year to year, ranging from over twenty to just one. The average is ten. The United States, Mexico, Central America, the Caribbean Islands and Canada are affected by storms in this basin. Forecasts for all storms are issued by the National Hurricane Center based in Miami, Florida; the Canadian Hurricane Centre, based in Halifax, Nova Scotia, also issues forecasts and warnings for storms expected to affect Canadian territory and waters. Hurricanes that strike Mexico, Central America, and Caribbean island nations, often do intense damage: they are deadlier when over warmer water, and the United States is better able to evacuate people from threatened areas than many other nations. Many of the more intense Atlantic storms are Cape Verde-type hurricanes, forming just west of Africa near the Cape Verde islands.

Unusual formation areas

The following areas spawn tropical cyclones only very rarely.

• Southern Atlantic Ocean: A combination of cooler waters, the lack of an Inter-tropical Convergence Zone, and wind shear makes it very difficult for the Southern Atlantic to support tropical activity. However, three tropical cyclones have been observed here — a weak tropical storm in 1991 off the coast of Africa, Cyclone Catarina (sometimes also referred to as Aldonça), which made landfall in Brazil in 2004, and a smaller storm in January of 2004, east of Salvador, Brazil. The January storm is thought to have reached tropical storm intensity based on scatterometre winds.
• Central North Pacific: Shear in this area of the Pacific Ocean severely limits tropical development. However, this region is commonly frequented by tropical cyclones that form in the much more favorable Eastern North Pacific Basin.
• Mediterranean Sea: Storms which appear similar to tropical cyclones in structure sometimes occur in the Mediterranean basin. Such cyclones formed in September 1947, September 1969, January 1982, September 1983, and January 1995. There is debate on whether these storms were tropical in nature.

Timing

Worldwide, tropical cyclone activity peaks in late summer when water temperatures are warmest. However, each particular basin has its own seasonal patterns.

In the north Atlantic, a distinct hurricane season occurs from June 1 to November 30, sharply peaking in early September. The northeast Pacific has a broader period of activity, but in a similar timeframe to the Atlantic. The northwest Pacific sees tropical cyclones year-round, with a minimum in February and a peak in early September. In the north Indian basin, storms are most common from April to December, with peaks in May and November.

In the southern hemisphere, tropical cyclone activity begins in late October, and ends in May. Southern hemisphere activity peaks in mid-February to early March.

Structure

A strong tropical cyclone consists of the following components.

• Surface low: All tropical cyclones rotate around an area of low atmospheric pressure near the earth's surface. The pressures recorded at the centers of tropical cyclones are among the lowest that occur on Earth's surface at sea level.
• Warm core: tropical cyclones are characterized and driven by the release of large amounts of latent heat of condensation as moist air is carried upwards and its water vapor condenses. This heat is distributed vertically, around the center of the storm. Thus, at any given altitude (except close to the surface where water temperature dictates air temperature) the environment inside the cyclone is warmer than its outer surroundings.
• Central Dense Overcast (CDO): The Central Dense Overcast is a dense shield of rain bands and thunderstorm activity surrounding the central low. Tropical cyclones with symmetrical CDO tend to be strong and well developed.
• Eye: A strong tropical cyclone will harbor an area of sinking air at the center of circulation. Weather in the eye is normally calm and free of clouds (however, the sea may be extremely violent). Eyes are home to the coldest temperatures of the storm at the surface, and the warmest temperatures at the upper levels. The eye is normally circular in shape, and may range in size from 8 km to 200 km (5 miles to 125 miles) in diameter. In weaker cyclones, the CDO covers the circulation center, resulting in no visible eye.
• Eyewall: The eyewall is a circular band of intense convection and winds immediately surrounding the eye. It is home to the most severe conditions in a tropical cyclone. Intense cyclones show eye-wall replacement cycles, in which outer eye walls form to replace inner ones. The mechanisms which make this occur are still not fully understood.
• Outflow: the upper levels of a tropical cyclone feature winds headed away from the center of the storm with an anticyclonic rotation. Winds at the surface are strongly cyclonic, weaken with height, and eventually reverse themselves. Tropical cyclones owe this unique characteristic to the warm core at the center of the storm.

Formation and development

The formation of tropical cyclones is still the topic of extensive research, and is still not fully understood. Five factors are necessary to make tropical cyclone formation possible:

1. Sea surface temperatures above 26.5 degrees Celsius to at least a depth of 50 meters. Warm waters are the energy source for tropical cyclones. When these storms move over land or cooler areas of water they weaken rapidly.
2. Upper level conditions must be conducive to thunderstorm formation. Temperatures in the atmosphere must decrease quickly with height, and the mid-troposphere must be relatively moist.
3. A pre-existing weather disturbance. This is most frequently provided by tropical waves - non rotating areas of thunderstorms which move through the world's tropical oceans.
4. A distance of approximately 10 degrees or more from the equator (2004's Hurricane Ivan, the strongest storm to be so far south, started its formation at 9.7 degrees north). The Coriolis Effect initiates and helps maintain the rotation of a tropical cyclone. The absence of this effect at and near the equator prohibits development.
5. Lack of vertical wind shear (change in wind velocity over height). High levels of wind shear can break apart the vertical structure of a tropical cyclone, prohibiting development.

Tropical cyclones can occasionally form despite not meeting these conditions. A combination of a pre-existing disturbance, upper level divergence, and a monsoon related cold spell led to the creation of Typhoon Vamei at only 1.5 degrees north of the equator in 2001. It is estimated that the factors leading to the formation of this typhoon occur only once every 400 years.

When a tropical cyclone reaches higher latitudes or passes over land, it may merge with weather fronts or develop into a frontal cyclone, also called extratropical cyclone. In the Atlantic ocean, such tropical-derived cyclones of higher latitudes can be violent and may occasionally remain at hurricane-force wind speeds when they reach Europe as a European windstorm.

Dissipation

A tropical cyclone can cease to have tropical characteristics in several ways:

• It moves over land, thus depriving it of the warm water it needs to power itself, and quickly loses strength. Most strong storms become disorganized areas of low pressure within a day or two of landfall. There is, however, a chance they could regenerate if they manage to get back over open warm water. If a storm is over mountains for even a short time, it can rapidly lose strength. This is, however, the cause of many storm fatalities, as the dying storm unleashes torrential rainfall, and in mountainous areas, this can lead to deadly mudslides.
• It remains in the same area of ocean for too long, consuming all the heat available and dissipating.
• It experiences wind shear, causing the convection to lose direction and the heat engine breaks down.
• It can be weak enough to be consumed by another area of low pressure, disrupting it and joining to become a large area of non-cyclonic thunderstorms.
• It enters colder waters. This does not necessarily mean the death of the storm, but the storm will lose its tropical characteristics. These storms are extratropical cyclones.

Even after a tropical cyclone is said to be extratropical or dissipated, it can still have gale-force winds and drop several inches of rainfall.

Attempts to dissipate cyclones

In the 1960's and 70's, the United States government attempted to weaken hurricanes in its Project Stormfury by seeding with silver iodide. It was thought that the seeding would cause changes in the structure of the hurricane, essentially disrupting the eyewall to collapse and thus reduce the winds. However, it was later determined that these eyewall replacement cycles happen naturally, and so the success of the program was impossible to gauge.

Observations

Intense tropical cyclones pose a particular observation challenge. As they are a dangerous oceanic phenomenon, weather stations are rarely available on the site of the storm itself, unless it is passing over an island or a coastal area, or an unfortunate ship is caught in the storm. Even in these cases, real-time measurement taking is generally only possible in the periphery of the cyclone, where conditions are less catastrophic.

It is however possible to take in-situ measurements, in real-time, by sending specially equipped reconnaissance flights into the cyclone. These are flown by four-engine turboprop aircraft, which take direct and remote-sensing measurements and launch dropsondes inside the cyclone.

The cyclone can also be imaged remotely by radar, and by weather satellites using visible light and infrared.

Effects

A mature tropical cyclone can release heat at a rate upwards of 6x10¹⁴ watts.[2] http://www.noaa.gov/questions/question_082900.html This is two hundred times the total rate of human electrical production, and is equivalent to detonating a 10 megaton nuclear bomb every 20 minutes. Tropical cyclones on the open sea cause large waves, heavy rain, and high winds, disrupting international shipping and sometimes sinking ships. However, the most devastating effects of a tropical cyclone occur when they cross coastlines, making landfall. A tropical cyclone moving over land can do direct damage in four ways.

• High winds - Hurricane strength winds can damage or destroy vehicles, buildings, bridges, etc. High winds also turn loose debris into flying projectiles, making the outdoor environment even more dangerous.
• Storm surge - Tropical cyclones cause an increase in sea level which can flood coastal communities. This is the worst effect, as cyclones claim 80% of their victims when they first strike shore.
• Heavy rain - The thunderstorm activity in a tropical cyclone causes intense rainfall. Rivers and streams flood, roads become impassable, and landslides can occur.
• Tornado activity - The broad rotation of a hurricane often spawns tornadoes. While these tornadoes are normally not as strong as their non-tropical counterparts, they can still cause tremendous damage.

Often, the secondary effects of a tropical cyclone are equally damaging. They include:

• Disease - The wet environment in the aftermath of a tropical cyclone, combined with the destruction of sanitation facilities and a warm tropical climate can induce epidemics of disease which claim lives long after the storm passes.
• Power outages - Tropical cyclones often knock out power to tens of thousands of people, prohibiting vital communication and hampering rescue efforts.
• Transportation difficulties - Tropical cyclones often destroy key bridges, overpasses, and roads, complicating efforts to transport food, clean water, and medicine to the areas that need it.

Beneficial effects of tropical cyclones

The human toll of cyclones cannot have a price put on it. However, cyclones may bring much-needed precipitation to otherwise dry regions. An appreciable percentage of Japan's rainfall is due to typhoons. Hurricane Camille averted drought conditions and ended water deficit s along much of its path. Additionally, the destruction caused by Camille on the Gulf coast spurred redevelopment, multiplying many times the land values that existed before the storm. However, disaster officials point out that this is not necessarily a good thing; it just encourages more people to live in what is clearly a danger area for deadly storms.

Additionally, hurricanes actually help to maintain global heat balance by moving warm, moist tropical air northward to the mid-latitudes and polar regions.

Notable cyclones

Main article: List of notable tropical cyclones

Tropical cyclones that cause massive destruction are fortunately rare, but when they happen, they can cause damage in the thousands of lives and the billions of dollars.

The deadliest tropical cyclone on record is a 100 mph (160 km/h, Category 2) storm that hit the densely populated Ganges Delta region of East Pakistan (now Bangladesh) on November 13, 1970. It killed anywhere from 200,000 to 500,000 people. The Indian Ocean basin has historically been the deadliest, with three storms since 1900 killing over 100,000 people each in Bangladesh. [3] http://encarta.msn.com/media_701500587_761565992_-1_1/Major_Hurricanes_Typhoons_
Cyclones_and_other_Storms_since_1900.html

In the Atlantic basin, three storms have killed more than 10,000 people. Hurricane Mitch during the 1998 Atlantic hurricane season caused severe flooding and mudslides in Honduras, killing at least 10,000 people and changing the landscape enough that entirely new maps of the nation were needed. The Galveston Hurricane of 1900, which made landfall at Galveston, Texas as an estimated category 4 storm, killed 6,000 to 12,000 people and remains the deadliest natural disaster in the history of the United States. The deadliest Atlantic storm on record was the Great Hurricane of 1780, which killed between 20 and 30 thousand people in the Antilles.

The most costly storm was 1992's Hurricane Andrew, which caused an estimated $25 billion in damage in Florida and the U.S. Gulf Coast, and remains the most destructive natural disaster in United States history.

The most intense storm on record was Typhoon Tip in the northwestern Pacific Ocean in 1979, which had a minimum pressure of only 870 mb and maximum sustained windspeeds of 190 mph (305 km/h). Fortunately, it weakened before striking Japan. Tip does not, however, hold alone the record for fastest sustained winds in a cyclone; Typhoon Keith in the Pacific, and Hurricane Camille and Hurricane Allen in the North Atlantic currently share this record as well [4] http://www.weatherwatchers.org/tropical/1998/13/mitch.html , although recorded windspeeds that fast are suspect, since most monitoring equipment is likely to be destroyed by such conditions.

Camille was the only storm to actually strike land while at that intensity, making it, with 190 mph (305 km/h) sustained winds and 210 mph (335 km/h) gusts, the strongest tropical cyclone of record to ever hit land. For comparison, these speeds are encounted at the center of a strong tornado, but Camille was much larger than any tornado.

Typhoon Nancy in 1961 had recorded windspeeds of 213 mph (343 km/h), but recent research indicates that windspeeds from the 1940s to the 1960s were gauged too high, and this is no longer considered the fastest storm on record. [5] http://www.aoml.noaa.gov/hrd/tcfaq/E1.html Similarly, a gust caused by Typhoon Paka over Guam was recorded at 236 mph (380 km/h); however, this reading had to be discarded, since the anemometer was damaged by the storm. Had it been confirmed, this would be the strongest wind ever recorded at the Earth's surface. (The current record is held by a non-hurricane wind registering 231 mph (372 km/h) at Mount Washington in New Hampshire.) [6] http://www.guam.navy.mil/weather.htm

Tip was also the largest cyclone on record, with a circulation of 1,350 miles (2,170 km) wide. The average tropical cyclone is only 300 miles (480 km) wide.[7] http://hurricanes.noaa.gov/prepare/structure.htm

Hurricane Iniki in 1992 was the most powerful storm to strike Hawaii in recorded history, hitting Kauai as a Category 4 hurricane, killing six and causing $3 billion in damage.

On December 25 1974, Tropical Cyclone Tracy hit Darwin, Australia. It was the most devastating natural disaster to have ever hit an Australian city, destroying around 70% of the homes in Darwin. Fifty people died in Darwin, and 16 at sea. Authorities had managed to evacuate most of Darwin. Although Cyclone Tracy was quite small — the smallest cyclone on record, in fact, little larger than 30 miles (48 km) wide — it was very severe, with winds of up to 135 mph (217 km/h). The damage was estimated to be close to $A400 million, which (at 2004 exchange rates) is approximately equal to $US 280 million.

On March 26, 2004, Cyclone Catarina became the first hurricane ever observed in the South Atlantic Ocean. Previous South Atlantic cyclones in 1991 and 2004 reached only tropical storm strength. Hurricanes may have formed there prior to 1960 but were not observed until weather satellites began monitoring the Earth's oceans in that year.

A tropical cyclone need not be particularly strong to cause memorable damage; Tropical Storm Allison in 2001 had its name retired for killing 41 people and causing over $5 billion damage in Texas, even though it never became a hurricane. Hurricane Jeanne in 2004 was only a tropical storm when it made a glancing blow on Haiti, but flooding and mudslides killed over 2,000 people.

Naming of tropical cyclones

Tropical cyclones with winds exceeding 17 metres per second are given names, to assist in recording insurance claims, to assist in warning people of the coming storm, and to further indicate that these are important storms that should not be ignored. These names are taken from lists which vary from region to region and are drafted a few years ahead of time. The lists are decided upon, depending on the regions, either by committees of the World Meteorological Organization (called primarily to discuss many other issues), or by national weather services involved in the forecasting of the storms.

Each year, the names of particularly destructive storms are "retired" and new names are chosen to take their place.

See also: Lists of tropical cyclone names

History of tropical cyclone naming

For several hundred years after the arrival of Europeans in the West Indies, hurricanes there were named after the saint's day on which the storm struck. During World War II, tropical cyclones were given female names, mainly for the convenience of the forecasters and in a somewhat ad hoc manner.

The modern naming convention came about in response to the need for unambiguous radio communications with ships and aircraft. As transportation traffic increased and meteorological observations improved in number and quality, several typhoons, hurricanes or cyclones might have to be tracked at any given time. To help in their identification, in the early 1950's the practice of systematically naming tropical storms and hurricanes was initiated by the United States National Hurricane Center, and is now maintained by the WMO.

In keeping with the common English language practice of referring to inanimate objects such as boats, trains, etc., using the female pronoun "she", names used were exclusively female. The first storm of the year was assigned a name beginning with the letter "A", the second with the letter "B", etc. However, since tropical storms and hurricanes are primarily destructive, some considered this practice Censored page. The National Weather Service responded to these concerns in 1979 with the introduction of male names to the nomenclature.

The naming process

The WMO's Regional Association IV Hurricane Committee selects the names for Atlantic Basin and central and eastern Pacific storms.

Currently, in the Atlantic and Eastern North Pacific regions, female and male names during a given season are assigned alternately, still in alphabetic order. The "gender" of the first storm of the season also alternates year to year. Six lists of names are prepared in advance, and reused on a six-year cycle (a different list is used for each year). Names of storms may be retired at the request of affected countries if they have caused extensive damage to life and property.

In the Central North Pacific region, the name lists are maintained by the Central Pacific Hurricane Center in Honolulu, Hawaii. Four lists of Hawaiian names are selected and used in sequential order without regard to year.

In the Western North Pacific, name lists are maintained by the WMO Typhoon Committee . Five lists of names are used, with each of the 14 nations on the Typhoon Committee submitting two names to each list. Names are used in the order of the countries' English names, sequentially without regard to year. Japan Meteorological Agency uses a secondary naming system in Western North Pacific that numbers a typhoon on the order it formed resetting on December 31 of every year. The Typhoon Songda in September 2004 is internally called the typhoon number 18 and is recorded as the typhoon 0418 with 04 taken from the year.

The Australian Bureau of Meteorology maintains three lists of names, one for each of the Western, Northern and Eastern Australian regions. There are also Fiji region and Papua New Guinea region names. The Seychelles Meteorological Service maintains a list for the Southwest Indian Ocean.

Etymology

• The word typhoon seems to be a result of collision between the Greek mythological monster Typhon and the Chinese phrase tai feng = "big wind".
• The word hurricane started as a name of a native Caribbean Amerindian storm god.
• The word cyclone came from the Greek word kyklos = "circle", "wheel".

See also

• Cyclone
• Arctic cyclone
• Beaufort scale
• Neutercane
• Polar low
• Project Stormfury
• Subtropical cyclone
• Extratropical
• List of Atlantic hurricane seasons

External links

• Canadian Hurricane Centre (Environment Canada) http://www.hurricanes.ca
• An excellent hurricane FAQ http://www.aoml.noaa.gov/hrd/tcfaq/tcfaqHED.html
• Global climatology of tropical cyclones http://www.bom.gov.au/bmrc/pubs/tcguide/ch1/ch1_3.htm
• Naming hurricanes http://www.nhc.noaa.gov/HAW2/english/basics/naming.shtml
• Unisys historical and contemporary hurricane track data http://weather.unisys.com/hurricane/ e.g. Atlantic 1968 http://weather.unisys.com/hurricane/atlantic/1968/index.html
• Worldwide tropical cyclone tracks, 1979-1988 http://www.bom.gov.au/bmrc/pubs/tcguide/ch1/figures_ch1/figure1.9.htm
• Worldwide tropical cyclone basins http://www.aoml.noaa.gov/hrd/tcfaq/6RSMCs.jpg
• Caribbean Hurricane Network http://www.stormcarib.com
• 1995 Mediterranean "Hurricane" http://www.mindspring.com/~jbeven/intr0008.htm
• Current Atlantic and Gulf of Mexico hurricane information http://a.www.orlandoweather.com/hurricanes/index.html
• Atlantic hurricane tracker Java applet http://html.wesh.com/sh/idi/weather/hurricanes/hurricanetracker.html
• UKMO leaflet on hurricanes http://www.meto.gov.uk/education/curriculum/leaflets/hurricanes.html
• Dates of Atlantic category 5 hurricanes http://lwf.ncdc.noaa.gov/oa/satellite/satelliteseye/educational/cat5hur.html
• WMO guide on cyclone terminology http://www.bom.gov.au/bmrc/pubs/tcguide/ch1/ch1_3.htm
• Tropical cyclone pictures and movies, from the United Kingdom Met Office http://www.metoffice.com/sec2/sec2cyclone/tcim.html
• Hurricanes explained http://www.guardian.co.uk/flash/0,5860,773980,00.html - Find out how they occur with this interactive guide from The Guardian http://www.guardian.co.uk (Uses Macromedia Flash http://www.macromedia.com/shockwave/download/index.cgi?P1_Prod_Version=Shockwave
  Flash )