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Deep Throat

The term Deep Throat has several meanings:

  • Deep Throat is a 1972 pornographic movie. This is the origin of all the other meanings of the term.
  • Deep throating is a sexual act, a type of fellatio depicted in the movie.
  • Deep Throat was the name given to the source in the Washington Post investigation of the Watergate scandal, revealed on May 31, 2005 to be former FBI associate director W. Mark Felt.
  • In general, the term Deep Throat has since been used for secret inside informers or whistleblowers.
  • Deep Throat is the pseudonym of several fictional characters who have acted as a whistleblower:
    • Deep Throat in the television series The X-Files.
    • Deep Throat is the alias of a character in Metal Gear Solid.
  • Deep Throat or Win32.DeepThroat is a computer virus
  • Inside Deep Throat is a 2005 documentary about the 1972 movie.

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The term Deep Throat has several meanings:. Before that, the most costly (in money, not human terms) storm had been 1992's Hurricane Andrew, which caused an estimated $25 billion in damage in Florida. Inside Deep Throat is a 2005 documentary about the 1972 movie. It is also estimated to have caused an estimated $40 to $120 billion in damages. Deep Throat or Win32.DeepThroat is a computer virus. Its death toll is above 1300, mainly from flooding and the aftermath. Deep Throat is the alias of a character in Metal Gear Solid. history.

Deep Throat in the television series The X-Files. National Hurricane Center, in its August review of the tropical storm season stated that Katrina is probably the worst natural disaster in U.S. Deep Throat is the pseudonym of several fictional characters who have acted as a whistleblower:

    . The U.S. In general, the term Deep Throat has since been used for secret inside informers or whistleblowers. On August 29, 2005, Hurricane Katrina made landfall in Louisiana and Mississippi. Mark Felt. Hurricane Jeanne in 2004 was only a tropical storm when it made a glancing blow on Haiti, but the flooding and mudslides it caused killed over 3,000 people.

    Deep Throat was the name given to the source in the Washington Post investigation of the Watergate scandal, revealed on May 31, 2005 to be former FBI associate director W. A tropical cyclone need not be particularly strong to cause memorable damage; Tropical Storm Allison in June 2001 had its name retired for killing 41 people and causing over $5 billion damage in East Texas, even though it never became a hurricane; the damage from Allison was mostly due to flooding, not winds or storm surge. Deep throating is a sexual act, a type of fellatio depicted in the movie. Hurricanes may have formed there prior to 1960 but were not observed until weather satellites began monitoring the Earth's oceans in that year. This is the origin of all the other meanings of the term. Previous South Atlantic cyclones in 1991 and 2004 reached only tropical storm strength. Deep Throat is a 1972 pornographic movie. On March 26, 2004, Cyclone Catarina became the first recorded South Atlantic hurricane.

    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. [18]. The smallest storm on record, 1974's Cyclone Tracy, which devastated Darwin, Australia, was roughly 30 miles (50 km) wide. The average tropical cyclone is only 300 miles (480 km) wide.

    Tip was also the largest cyclone on record, with a circulation 1,350 miles (2,170 km) wide. (The current record is held by a non-hurricane wind registering 231 mph (372 km/h) at Mount Washington in New Hampshire.) [17]. Had it been confirmed, this would be the strongest non-tornadic wind ever recorded at the Earth's surface. [16] 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.

    Typhoon Nancy in 1961 had recorded wind speeds of 213 mph (343 km/h), but recent research indicates that wind speeds from the 1940s to the 1960s were gauged too high, and this is no longer considered the fastest storm on record. For comparison, these speeds are encountered at the center of a strong tornado, but Camille was much larger and long-lived than any tornado. 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. Tip does not hold the record for fastest sustained winds in a cyclone alone; Typhoon Keith in the Pacific, and Hurricane Camille and Hurricane Allen in the North Atlantic currently share this record as well [15], although recorded wind speeds that fast are suspect, since most monitoring equipment is likely to be destroyed by such conditions.

    It weakened before striking Japan. The most intense storm on record was Typhoon Tip in the northwestern Pacific Ocean in 1979, which had a minimum pressure of only 870 mbar and maximum sustained wind speeds of 190 mph (305 km/h). The deadliest Atlantic storm on record was the Great Hurricane of 1780, which killed about 22,000 people in the Antilles. The Galveston Hurricane of 1900, which made landfall at Galveston, Texas as an estimated Category 4 storm, killed 8,000 to 12,000 people, and remains the deadliest natural disaster in the history of the United States.

    Hurricane Mitch during the 1998 Atlantic hurricane season caused severe flooding and mudslides in Honduras, killing about 18,000 people and changing the landscape enough that entirely new maps of the country were needed. In the Atlantic basin, at least two storms have killed more than 10,000 people. [14]. The North Indian basin has historically been the deadliest, with three storms since 1900 killing over 100,000 people, each in Bangladesh.

    It killed an estimated 500,000 people. The deadliest tropical cyclone on record hit the densely populated Ganges Delta region of East Pakistan (now Bangladesh) on November 13, 1970, likely as a Category 3 tropical cyclone. 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. This statistic needs refining because the variables being tested are not normally distributed with equal variances, but it may provide the best evidence yet that the impact of global warming on hurricane intensity has been detected.

    Under the assumption that the six basins are statistically independent except for the effect of global warming, Stoft has carried out the obvious paired t-test and found that the null-hypothesis of no impact of global warming on the percentage of category 4 & 5 hurricanes can be rejected at the 0.1% level—there is only a 1 in 1000 chance of simultaneously finding the observed six increases in the cat-4&5 percentages. do not undertake any such test. Unfortunately Webster et al. But if the local oscillations are not synchronized by some as-yet-unidentified global oscillation, the independence of the basins allows joint statistical tests that are more powerful than any set of individual basin tests.

    Because each individual basin may be subject to intra-basin oscillations similar to the AMO, any single-basin statistic remains open to question. analyze the slightly less relevant percentage of hurricanes in the combined categories 4 and 5, and find that this percentage has increased in each of six distinct hurricane basins: North Atlantic, North East and North West Pacific, South Pacific, and North and South Indian. While Emanuel analyzes total annual energy dissipation, Webster et al. [13].

    So, both a natural variation (such as the AMO) and global warming could have made contributions to the warming of the tropical Atlantic over the past decades, but an exact attribution is so far impossible to make. Emanuel, however, found the recent temperature increase was outside the range of previous oscillations. K. The question then becomes: what caused the observed increase in sea surface temperatures? In the Atlantic, it could be due to the Atlantic Multidecadal Oscillation (AMO), a 50–70 year pattern of temperature variability.

    Both Emanuel and Webster et al., consider the sea surface temperature as of key importance in the development of cyclones. I.e., while the number of cyclones decreased overall, the number of very strong cyclones increased. The main finding is that while the number of cyclones "decreased in all basins except the North Atlantic during the past decade" there is a "large increase in the number and proportion of hurricanes reaching categories 4 and 5". published an article in Science 309, 1844-1846 examining "changes in tropical cyclone number, duration, and intensity" over the last 35 years, a period where satellite data is available.

    Webster et al. Along similar lines, P.J. Emanuel further predicts "a substantial increase in hurricane-related losses in the twenty-first century". Emanuel states that the potential hurricane destructiveness, a measure which combines strength, duration, and frequency of hurricanes, "is highly correlated with tropical sea surface temperature, reflecting well-documented climate signals, including multidecadal oscillations in the North Atlantic and North Pacific, and global warming." K.

    In this article, K. Emanuel (2005) (Nature 436, 686–688, preprint). This consensus is now questioned by K. Regarding strength, a similar conclusion was consensus until recently.

    National Oceanic and Atmospheric Administration says in their Hurricane FAQ that "it is highly unlikely that global warming has (or will) contribute to a drastic change in the number or intensity of hurricanes." [12]. The U.S. The question is thus whether a statistical trend in frequency or strength of cyclones exists. So far, virtually all climatologists seem to agree that a single storm, or even a single season, cannot clearly be attributed to a single cause such as global warming or natural variation [11].

    A common question is whether global warming can or will cause more frequent or more fierce tropical cyclones. The official record, therefore, probably misses many storms in which no ship experienced gale-force winds, recognized it as a tropical storm (as opposed to a high-latitude extra-tropical cyclone, a tropical wave, or a brief squall), returned to port, and reported the experience. Before the satellite era began in 1961, tropical storms or hurricanes went undetected unless a ship reported a voyage through the storm. These unusually active hurricane seasons predated satellite coverage of the Atlantic basin that now enables forecasters to see all tropical cyclones.

    Few hurricanes occurred in the 1840s to 1860s; however, many struck in the early 1800s, including an 1821 storm that made a direct hit on New York City which some historical weather experts say may have been as high as Category 4 in strength. During the 1887 season, 19 tropical storms formed, of which a record 4 occurred after 1 November and 11 strengthened into hurricanes. Tropical hurricanes occurred infrequently during the seasons of 1900-1925; however, many intense storms formed 1870-1899. A record 21 Atlantic tropical storms formed in 1933, only recently exceeded in 2005.

    Destructive hurricanes struck frequently from 1926-60, including many major New England hurricanes. Although more common since 1995, few above-normal hurricane seasons occurred during 1970-1994. The number and strength of Atlantic hurricanes may undergo a 50-70-year cycle. Although the record shows a distinct increase in the number and strength of intense hurricanes, therefore, experts regard the early data as suspect.

    The combined effects of ship destruction and remote landfall severely limit the number of intense hurricanes in the official record before the era of hurricane reconnaissance aircraft and satellite meteorology. Often in part because of the threat of hurricanes, many coastal regions had sparse population between major ports until the advent of automobile tourism; therefore, the most severe portions of hurricanes striking the coast often went unmeasured. This can to a large extent be attributed to the number of people living in susceptible coastal area, and massive development in the region since the last surge in Atlantic hurricane activity in the 1960s. Atlantic storms are certainly becoming more destructive financially, since five of the ten most expensive storms in United States history have occurred since 1990.

    [10]. While the number of storms in the Atlantic has increased since 1995, there seems to be no signs of a global trend; the annual global number of tropical cyclones remains about 90 ± 10. James Lovelock has also hypothesised that by raising nutrients from the sea floor to surface layers of the ocean, hurricanes also increase biological activity in areas where life would be difficult through nutrient loss in the deeper reaches of the ocean. Hurricanes also help to maintain global heat balance by moving warm, moist tropical air to the mid-latitudes and polar regions.

    Of course, many former residents and businesses do relocate to inland areas away from the threat of future hurricanes as well. On the other hand, disaster response officials point out that redevelopment encourages more people to live in clearly dangerous areas subject to future deadly storms (as shown by the effects of Hurricane Katrina). The destruction caused by Camille on the Gulf coast spurred redevelopment as well, greatly increasing local property values. Hurricane Floyd did the same thing in New Jersey in 1999.

    Hurricane Camille averted drought conditions and ended water deficits along much of its path. Hurricane Allen ended the Texas drought of 1980. Although cyclones take an enormous toll in lives and personal property, they may bring much-needed precipitation to otherwise dry regions. They include:.

    Often, the secondary effects of a tropical cyclone are equally damaging. A tropical cyclone moving over land can do direct damage in four ways. However, the most devastating effects of a tropical cyclone occur when they cross coastlines, making landfall. Tropical cyclones on the open sea cause large waves, heavy rain, and high winds, disrupting international shipping and sometimes sinking ships.

    A mature tropical cyclone can release heat at a rate upwards of 6x1014 watts [9]. Example: Ken-Lola (1989). Sometimes, there may be human faults leading to the renaming of a tropical cyclone. Human faults.

    4. Example: TD 10-TD 12 (2005). When the remnants of a tropical cyclone redevelop, the redeveloping system will be treated as a new tropical cyclone if there are uncertainties of the continuation, even though the original system may contribute to the forming of the new system. Uncertainties of the continuation.

    3. Up to now, there has been no tropical cyclone retaining its name during the passage from Atlantic to Pacific, or vice versa. In 2003, when Larry was about to move across Mexico, NHC attempted to provide greater clarity:. NHC explained that Iris had dissipated as a tropical cyclone prior to entering the eastern North Pacific basin; the new depression was properly named Fifteen-E, rather than Iris.

    The depression later became tropical storm Manuel. However, the Pacific tropical depression developed from the remnants of Iris was called Fifteen-E instead. In 2001, when Iris moved across Central America, NHC mentioned that Iris would retain its name if it regenerated in the Pacific. Examples: Cesar-Douglas (1996), Joan-Miriam (1988).

    It was the policy of National Hurricane Center (NHC) to rename a tropical storm which crossed from Atlantic into Pacific, or vice versa. A tropical storm crosses from the Atlantic into the Pacific, or vice versa, before 2001. 2. Examples: Bertie-Alvin (2005).

    In this case, the Joint Typhoon Warning Center (JTWC) will put two names together with a hyphen. In the south Indian Ocean, RSMC la Reunion names a tropical storm once it crosses 90°E from the east, even though it has been named. A tropical storm enters the southwestern Indian Ocean from the east. 1.

    However, a tropical cyclone may be renamed in several occasions. In most cases, a tropical cyclone retains its name throughout its life. The names are usually of English, French or Spanish origin in the Atlantic basin, since these are the three predominant languages of the region where the storms typically form. It was also in 1979 that the practice of preparing a list of names before the season began.

    The National Weather Service responded to these concerns in 1979 with the introduction of masculine names to the nomenclature. However, since tropical storms and hurricanes are primarily destructive, some considered this practice sexist. The first storm of the year was assigned a name beginning with the letter "A", the second with the letter "B", etc. 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 feminine.

    To help in their identification, beginning in 1953 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. 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. The modern naming convention came about in response to the need for unambiguous radio communications with ships and aircraft. For a few years afterwards, names from the Joint Army/Navy Phonetic Alphabet were used.

    During World War II, tropical cyclones were given feminine names, mainly for the convenience of the forecasters and in a somewhat ad hoc manner. He used feminine names, the names of politicians who had offended him, and names from history and mythology. The practice of giving storms people's names was introduced by Clement Lindley Wragge, an Anglo-Australian meteorologist at the end of the 19th century. For several hundred years after Europeans arrived in the West Indies, hurricanes there were named after the saint's day on which the storm struck.

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

    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. Names are used in the order of the countries' English names, sequentially without regard to year. Five lists of names are used, with each of the 14 nations on the Typhoon Committee submitting two names to each list. In the Western North Pacific, name lists are maintained by the WMO Typhoon Committee.

    Four lists of Hawaiian names are selected and used in sequential order without regard to year. In the Central North Pacific region, the name lists are maintained by the Central Pacific Hurricane Center in Honolulu, Hawaii. There is no precedent for a storm named with a Greek Letter causing enough damage to justify retirement; how this situation would be handled is unknown. This was first necessary during the 2005 season when the names Alpha, Beta, Gamma, Delta, Epsilon, and Zeta were all used.

    If there are more than 21 named storms in an Atlantic season or 24 named storms in an Eastern Pacific season, the rest are named as letters from the Greek alphabet: the 22nd storm is called "Alpha," the 23rd "Beta," and so on. The affected countries then decide on a replacement name of the same gender (and if possible, the same ethnicity) as the name being retired. Names of storms may be retired by request of affected countries if they have caused extensive damage. Five letters — "Q," "U," "X," "Y" and "Z" — are omitted in the Atlantic; only "Q" and "U" are omitted in the Eastern Pacific, so the format accommodates 21 or 24 named storms in a hurricane season.

    Six lists of names are prepared in advance, and each list is used once every six years. The "gender" of the season's first storm also alternates year to year: the first storm of an odd-numbered year gets feminine name, while the first storm of an even-numbered year gets a masculine name. In the Atlantic and Eastern North Pacific regions, feminine and masculine names are assigned alternately in alphabetic order during a given season. The WMO's Regional Association IV Hurricane Committee selects the names for Atlantic Basin and central and eastern Pacific storms.

    Each year, the names of particularly destructive storms (if there were any) are "retired" and new names are chosen to take their place. 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. These names are taken from lists which vary from region to region and are drafted a few years ahead of time. Storms reaching tropical storm strength (winds exceeding 17 metres per second, 38 mph, or 62 km/h) 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.

    The National Hurricane Center uses the data to evaluate conditions at landfall and to verify forecasts. During landfall, the NOAA Hurricane Research Division compares and verifies data from reconnaissance aircraft (which includes wind speed data taken at flight level and from GPS dropwindsondes and stepped-frequency microwave radiometers) to wind speed data transmitted in real time from weather stations erected near or at the coast. The two largest programs are the Florida Coastal Monitoring Program [7] and the Wind Engineering Mobile Instrumented Tower Experiment [8]. Recently, academic researchers have begun to deploy mobile weather stations fortified to withstand hurricane-force winds.

    Radar plays a crucial role around landfall because it shows a storm's location and intensity minute by minute. As a storm approaches land, it can be observed by land-based Doppler radar. Tropical cyclones far from land are tracked by weather satellites capturing visible and infrared images from space, usually at half-hour to quarter-hour intervals. This demonstrated a new way to probe the storms at low altitudes that human pilots seldom dare[6].

    A new era in hurricane observation began when a remotely piloted Aerosonde, a small drone aircraft, was flown through Tropical Storm Ophelia as it passed Virginia's Eastern Shore during the 2005 hurricane season. These sondes measure temperature, humidity, pressure, and especially winds between flight level and the ocean's surface. The aircraft also launch GPS dropsondes inside the cyclone. These aircraft fly directly into the cyclone and take direct and remote-sensing measurements.

    The aircraft used are WC-130 Hercules and WP-3D Orions, both four-engine turboprop cargo aircraft. In the Atlantic basin, these flights are regularly flown by US government hurricane hunters [5]. It is however possible to take in-situ measurements, in real-time, by sending specially equipped reconnaissance flights into the cyclone. Even in these cases, real-time measurement taking is generally possible only in the periphery of the cyclone, where conditions are less catastrophic.

    Surface level observations are generally available only if the storm is passing over an island or a coastal area, or it has overtaken an unfortunate ship. As they are a dangerous oceanic phenomenon, weather stations are rarely available on the site of the storm itself. Intense tropical cyclones pose a particular observation challenge. However, it has been suggested by some that we can change the course of a storm during its early stages of formation, (detailed by an article, Controlling Hurricanes, Scientific American, 2005), such as using satellite to alter the environmental conditions or, more realistically, spreading degradable film of oil over the ocean, which prevent water vapor from fueling the storm.

    These approaches all suffer from the same flaw: tropical cyclones are simply too large for any of them to be practical [4]. Other approaches have been suggested over time, including cooling the water under a tropical cyclone by towing icebergs into the tropical oceans; dropping large quantities of ice into the eye at very early stages so that latent heat is absorbed by ice at the entrance (storm cell perimeter bottom) instead of heat energy being converted to kinetic energy at high altitudes vertically above; covering the ocean in a substance that inhibits evaporation; or blasting the cyclone apart with nuclear weapons. Today it is known that silver iodide seeding is not likely to have an effect because the amount of supercooled water in the rainbands of a tropical cyclone is too low.[3]. The project was dropped after it was discovered that eyewall replacement cycles occur naturally in strong hurricanes, casting doubt on the result of the earlier attempts.

    Because there was so much uncertainty about the behavior of these storms, the federal government would not approve seeding operations unless the hurricane had a less than 10 percent chance of making landfall within 48 hours. In an earlier episode, disaster struck when a hurricane east of Jacksonville, Florida, was seeded, promptly changed its course, and smashed into Savannah, Georgia[citation needed]. The winds of Hurricane Debbie dropped as much as 30 percent, but then regained their strength after each of two seeding forays. It was thought that the seeding would cause supercooled water in the outer rainbands to freeze, causing the inner eyewall to collapse and thus reducing the winds.

    In the 1960s and 1970s, the United States government attempted to weaken hurricanes in its Project Stormfury by seeding selected storms with silver iodide. 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. 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. Even after a tropical cyclone is said to be extratropical or dissipated, it can still have tropical storm force (or occasionally hurricane force) winds and drop several inches of rainfall.

    A tropical cyclone can cease to have tropical characteristics in several ways:. For a list of notable and unusual landfalling hurricanes, see list of notable tropical cyclones. For emergency preparedness, actions should be timed from when a certain wind speed will reach land, not from when landfall will occur. In fact, for a storm moving inland, the landfall area experiences half the storm before the actual landfall.

    Naturally, storm conditions may be experienced on the coast and inland well before landfall. Officially, "landfall" is when a storm's center (the center of the eye, not its edge) reaches land. They attribute the lack of improvement in intensity forecasting to the complexity of tropical systems and an incomplete understanding of factors that affect their development. But while track forecasts have become more accurate than 20 years ago, scientists say they are less skillful at predicting the intensity of tropical cyclones.

    High-speed computers and sophisticated simulation software allow forecasters to produce computer models that forecast tropical cyclone tracks based on the future position and strength of high- and low-pressure systems. With their understanding of the forces that act on tropical cyclones, and a wealth of data from earth-orbiting satellites and other sensors, scientists have increased the accuracy of track forecasts over recent decades. Because of the forces that affect tropical cyclone tracks, accurate track predictions depend on determining the position and strength of high- and low-pressure areas, and predicting how those areas will change during the life of a tropical system. East Coast and in the Gulf of Mexico are eventually forced toward the northeast by high-pressure areas which move from west to east over North Africa.

    Many tropical cyclones along the coast. Such a track direction change is termed recurve. A hurricane moving from the Atlantic toward the Gulf of Mexico, for example, will recurve to the north and then northeast if it encounters winds blowing northwestward toward a high-pressure system passing over North Africa. Finally, when a tropical cyclone moves into higher latitude, its general track around a high-pressure area can be deflected significantly by winds moving toward a low-pressure area. (Much of that is due to the conservation of angular momentum - air is drawn in from an area much larger than the cyclone such that the tiny angular velocity of that air will be magnified greatly when the distance to the storm center shrinks.).

    The Coriolis acceleration also initiates cyclonic rotation, but it is not the driving force that brings this rotation to high speeds. Thus, tropical cyclones in the Northern Hemisphere, which commonly move west in the beginning, normally turn north (and are then usually blown east), and cyclones in the Southern Hemisphere are deflected south, if no strong pressure systems are counteracting the Coriolis Acceleration. The southern part is pulled south, but since it is closer to the equator, the Coriolis force is a bit weaker there). in the north, the northern part of the cyclone has winds to the west, and the Coriolis force pulls them slightly north.

    This acceleration causes cyclonic systems to turn towards the poles in the absence of strong steering currents (i.e. The earth's rotation also imparts an acceleration (termed the Coriolis Acceleration or Coriolis Effect). Also, in the area of the North Atlantic where hurricanes form, trade winds, which are prevailing westward-moving wind currents, steer tropical waves (precursors to tropical depressions and cyclones) westward from off the African coast toward the Caribbean and North America. Over the North Atlantic Ocean, tropical systems are steered generally westward by the east-to-west winds on the south side of the Bermuda High, a persistent high-pressure area over the North Atlantic.

    The major force affecting the track of tropical systems in all areas are winds circulating around high-pressure areas. The path of motion is referred to as a tropical cyclone's track.. That is, large-scale winds—the streams in the earth's atmosphere—are responsible for moving and steering tropical cyclones. Although tropical cyclones are large systems generating enormous energy, their movements over the earth's surface are often compared to that of leaves carried along by a stream.

    In British Shipping Forecasts, winds of force 12 on the Beaufort scale are described as "hurricane force.". However, two powerful extratropical cyclones that ravaged France, Germany, and the United Kingdom in December 1999, "Lothar" and "Martin", were named due to their unexpected power (equivalent to a category 1 or 2 hurricane). These European windstorms can generate hurricane-force winds but are not given individual names. 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.

    Although subtropical storms rarely attain hurricane-force winds, they may become tropical in nature as their core warms. They can form in a wide band of latitude, from the equator to 50°. A subtropical cyclone is a weather system that has some characteristics of a tropical cyclone and some characteristics of an extratropical cyclone. Extratropical cyclones can also be dangerous because their low-pressure centers cause powerful winds.

    From space, extratropical storms have a characteristic "comma-shaped" cloud pattern. A tropical cyclone can become extratropical as it moves toward higher latitudes if its energy source changes from heat released by condensation to differences in temperature between air masses; more rarely, an extratropical cyclone can transform into a subtropical storm, and from there into a tropical cyclone. An extratropical cyclone is a storm that derives energy from horizontal temperature differences, which are typical in higher latitudes. Several of these relate to the formation or dissipation of tropical cyclones.

    Many other forms of cyclone can form in nature. weather service defines sustained winds based on 1-minute average speed measured about 10 meters (33 ft) above the surface. The U.S. The definition of sustained winds recommended by the World Meteorological Organization (WMO) and used by most weather agencies is that of a 10-minute average.

    The Joint Typhoon Warning Center classifies typhoons with wind speeds of at least 150 mi/h (67 m/s or 241 km/h, equivalent to a strong Category 4 storm) as Super Typhoons. The National Hurricane Center classifies hurricanes of Category 3 and above as Major Hurricanes. In fact, tropical systems of less than hurricane strength can produce significant damage and human casualties, especially from flooding and landslides. For instance, a Category 2 hurricane that strikes a major urban area will likely do more damage than a large Category 5 hurricane that strikes a mostly rural region.

    Lower-category storms can inflict greater damage than higher-category storms, depending on factors such as local terrain and total rainfall. The rankings are not absolute in terms of effects. A Category 1 storm has the lowest maximum winds, a Category 5 hurricane has the highest. Hurricanes are ranked according to their maximum winds using the Saffir-Simpson Hurricane Scale.

    Eventually the outer eyewall replaces the inner one completely and the storm can be the same intensity as it was previously or, in some cases, even stronger. the maximum winds die off a bit and the central pressure goes up). During this phase, the tropical cyclone is weakening (i.e. At this point, some of the outer rainbands may organize into an outer ring of thunderstorms that slowly moves inward and robs the inner eyewall of its needed moisture and momentum.

    When cyclones reach peak intensity they usually - but not always - have an eyewall and radius of maximum winds that contract to a very small size, around 5 to 15 miles. Eyewall replacement cycles naturally occur in intense tropical cyclones. Intense, mature hurricanes can sometimes exhibit an inward curving of the eyewall top that resembles a football stadium: this phenomenon is thus sometimes referred to as stadium effect. Maximum sustained winds in the strongest tropical cyclones have been measured at more than 85 m/s (165 knots, 190 mph, 305 km/h).

    The direction of the cyclonic circulation depends on the hemisphere; it is counterclockwise in the Northern Hemisphere, clockwise in the Southern Hemisphere. Bands or arms may extend over great distances as clouds are drawn toward the cyclone. The circulation of clouds around a cyclone's center imparts a distinct spiral shape to the system. Surrounding the eye is the eyewall, an area about 10 to 50 miles (16 to 80 kilometers) wide in which the strongest thunderstorms and winds circulate around the storm's center.

    The eye is often visible in satellite images as a small, circular, cloud-free spot. At hurricane and typhoon intensity, a tropical cyclone tends to develop an eye, an area of relative calm (and lowest atmospheric pressure) at the center of the circulation. Government weather services assign first names to systems that reach this intensity (thus the term named storm). At this point, the distinctive cyclonic shape starts to develop, though an eye is usually not present.

    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 (34–63 knots, 39–73 mph, or 62–117 km/h). It is already becoming a low-pressure system, however, hence the name "depression". It has no eye, and does not typically have the spiral shape of more powerful storms. 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).

    Tropical cyclones are classified into three main groups: tropical depressions, tropical storms, and a third group whose name depends on the region. A strong tropical cyclone consists of the following components. The following areas spawn tropical cyclones only very rarely. There are seven main basins of tropical cyclone formation:.

    It is estimated that such conditions occur only once every 400 years. A combination of a pre-existing disturbance, upper level divergence and a monsoon-related cold spell led to Typhoon Vamei at only 1.5 degrees north of the equator in 2001. Hurricane Ivan of 2004 developed within 10 degrees of the equator. These conditions are extremely rare, and such storms are believed to form at most once per century.

    However, it is possible for tropical cyclones to form within this boundary if there is another source of initial rotation. Because the Coriolis effect initiates and maintains tropical cyclone rotation, such cyclones almost never form or move within about 10 degrees of the equator [2], where the Coriolis effect is weakest. Nearly all of them form between 10 and 30 degrees of the equator and 87% form within 20 degrees of it. Most tropical cyclones form in a worldwide band of thunderstorm activity called the Intertropical convergence zone (ITCZ).

    Worldwide, an average of 80 tropical cyclones form each year. Southern Hemisphere activity peaks in mid-February to early March. In the Southern Hemisphere, tropical cyclone activity begins in late October and ends in May. In the North Indian basin, storms are most common from April to December, with peaks in May and November.

    The Northwest Pacific sees tropical cyclones year-round, with a minimum in February and a peak in early September. The Northeast Pacific has a broader period of activity, but in a similar timeframe to the Atlantic. The statistical peak of the North Atlantic hurricane season is September 10. In the North Atlantic, a distinct hurricane season occurs from June 1 to November 30, sharply peaking from late August through September.

    However, each particular basin has its own seasonal patterns. Worldwide, tropical cyclone activity peaks in late summer when water temperatures are warmest. These include:. Only specific weather disturbances can result in tropical cyclones.

    Tropical cyclones occasionally form despite not meeting these conditions. Five factors are necessary to make tropical cyclone formation possible:. The formation of tropical cyclones is the topic of extensive ongoing research, and is still not fully understood. The high cirrus clouds may be the first signs of an approaching hurricane.

    This outflow produces high, thin cirrus clouds that spiral away from the center. These originate from air that has released its moisture and is expelled at high altitude through the "chimney" of the storm engine. While the most obvious motion of clouds is toward the center, tropical cyclones also develop an upper-level (high-altitude) outward flow of clouds. Scientists at the National Center for Atmospheric Research estimate that a hurricane releases heat energy at the rate of 50 to 200 trillion watts -- about the amount of energy released by exploding a 10-megaton nuclear bomb every 20 minutes [1].

    As a result, when a tropical cyclone passes over land, its strength diminishes rapidly. The evaporation of this moisture is accelerated by the high winds and reduced atmospheric pressure in the storm, resulting in a positive feedback loop. In order to continue to drive its heat engine, a tropical cyclone must remain over warm water, which provides the atmospheric moisture needed. By contrast, mid-latitude cyclones, for example, draw their energy mostly from pre-existing horizontal temperature gradients in the atmosphere.

    Condensation as a driving force is what primarily distinguishes tropical cyclones from other meteorological phenomena, and because this is strongest in a tropical climate, this defines the initial domain of the tropical cyclone. If the right conditions persist and allow it to create a feedback loop by maximizing the energy intake possible, for example, such as high winds to increase the rate of evaporation, they can combine to produce the violent winds, incredible waves, torrential rains, and floods associated with this phenomenon. The factors to form a tropical cyclone include a pre-existing weather disturbance, warm tropical oceans, moisture, and relatively light winds aloft. The orbital revolution of the Earth causes the system to spin, an effect known as the Coriolis force, giving it a cyclone characteristic and affecting the trajectory of the storm.

    Factors such as a continued lack of equilibrium in air mass distribution would also give supporting energy to the cyclone. This gives rise to factors that give the system enough energy to be self-sufficient and cause a positive feedback loop where it can draw more energy as long as the source of heat, warm water, remains. Continued condensation leads to higher winds, continued evaporation, and continued condensation, feeding back into itself. Therefore, a tropical cyclone can be thought of as a giant vertical heat engine supported by mechanics driven by physical forces such as the rotation and gravity of the Earth.

    Its primary energy source is the release of the heat of condensation from water vapor condensing at high altitudes, the heat ultimately derived from the sun. Structurally, a tropical cyclone is a large, rotating system of clouds, wind and thunderstorms. [citation needed]. The word cyclone is from the Greek "κύκλος", meaning "circle." An Egyptian word Cykline meaning to "to spin" has been cited as a possible origin.

    The word hurricane is derived from the name of a native Caribbean Amerindian storm god, Huracan, via Spanish huracán. See tuphōn for more information. Portuguese tufão is also related to typhoon. The word typhoon has two possible origins:.

    There are many regional names for tropical cyclones, including Bagyo in the Philippines and Taino in Haiti. Terms used in weather reports for tropical cyclones that have surface winds over 64 knots (73.6 mph) or 32 m/s vary by region:. . While they can be highly destructive, tropical cyclones are an important part of the atmospheric circulation system, which moves heat from the equatorial region toward the higher latitudes.

    In meteorology, a tropical cyclone (also referred to as a tropical depression, tropical storm, typhoon, or hurricane depending on strength and geographical context) is a type of low pressure system which generally forms in the tropics. 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. Power outages - Tropical cyclones often knock out power to tens or hundreds of thousands of people (or occasionally millions if a large urban area is affected), prohibiting vital communication and hampering rescue efforts. Infections of cuts and bruises can be greatly amplified by wading in sewage-polluted water.

    One of the most common post-hurricane injuries is stepping on a nail in storm debris, leading to a risk of tetanus or other infection. 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. While these tornadoes are normally not as strong as their non-tropical counterparts, they can still cause tremendous damage. Tornado activity - The broad rotation of a hurricane often spawns tornadoes.

    Rivers and streams flood, roads become impassable, and landslides can occur. Heavy rain - The thunderstorm activity in a tropical cyclone causes intense rainfall. This is the worst effect, as cyclones claim 80% of their victims when they first strike shore. Storm surge - Tropical cyclones cause an increase in sea level, which can flood coastal communities.

    High winds also turn loose debris into flying projectiles, making the outdoor environment even more dangerous. High winds - Hurricane strength winds can damage or destroy vehicles, buildings, bridges, etc. Such weakening is generally temporary unless it meets other conditions above. An outer eye wall forms (typically around 50 miles from the center of the storm), choking off the convection toward the inner eye wall.

    These storms are extratropical cyclones. This does not necessarily mean the death of the storm, but the storm will lose its tropical characteristics. It enters colder waters. (Such, however, can strengthen the non-tropical system as a whole.).

    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 experiences wind shear, causing the convection to lose direction and the heat engine to break down. Without warm surface water, the storm cannot survive. It remains in the same area of ocean for too long, drawing heat off of the ocean surface until it becomes too cool to support the storm.

    However, many storm fatalities occur in mountainous terrain, as the dying storm unleashes torrential rainfall which can lead to deadly floods and mudslides. If a storm is over mountains for even a short time, it can rapidly lose its structure. There is, however, a chance they could regenerate if they manage to get back over open warm water. Most strong storms lose their strength very rapidly after landfall, and become disorganized areas of low pressure within a day or two.

    It moves over land, thus depriving it of the warm water it needs to power itself, and quickly loses strength. Tropical cyclones owe this unique characteristic to the warm core at the center of the storm. Winds at the surface are strongly cyclonic, weaken with height, and eventually reverse themselves. Outflow: The upper levels of a tropical cyclone feature winds headed away from the center of the storm with an anticyclonic rotation.

    The heaviest wind damage occurs where a hurricane's eyewall passes over land. Eyewall: A band around the eye of greatest wind speed, where clouds reach highest and precipitation is heaviest. In weaker cyclones, the CDO covers the circulation center, resulting in no visible eye. 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.

    Eyes are home to the coldest temperatures of the storm at the surface, and the warmest temperatures at the upper levels. Weather in the eye is normally calm and free of clouds (however, the sea may be extremely violent). Eye: A strong tropical cyclone will harbor an area of sinking air at the center of circulation. The classic hurricane contains a symmetrical CDO, which means that it is perfectly circular and round on all sides.

    This contains the eye wall, and the eye itself. Central Dense Overcast (CDO): The Central Dense Overcast is a dense shield of very intense thunderstorm activity that make up the inner portion of the hurricane. 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. This heat is distributed vertically, around the center of the storm.

    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. The pressures recorded at the centers of tropical cyclones are among the lowest that occur on Earth's surface at sea level. Surface low: All tropical cyclones rotate around an area of low atmospheric pressure near the Earth's surface. The Great Lakes A storm system that appeared similar to a tropical cyclone formed in 1996 on Lake Huron it formed an eye and could have breifly been sub-tropical.

    It formed from a thunderstorm formation in Borneo that moved into the South China Sea. It caused flooding in southern Malaysia and some damage in Singapore. However, in December 2001, Typhoon Vamei formed in the Southern South China Sea and made landfall in Malaysia. Areas within ten degrees laditude of the equator do not experience a significant coriolis force, a vital ingredient in tropical cyclone formation.

    Southern South China Sea Tropical cyclones normally do not develop in the Southern South China Sea due to its close proximity to the equator. Australia: SE Indian Basin includes the eastern part of the Indian ocean and the northern and western part of the Australian basin. Australia: SW Pacific Basin includes the eastern part of Australia and the Fiji area. before being transformed into an extratropical low or absorbed into other systems of low pressure.

    Vince's origin was the northernmost in the eastern Atlantic ever recorded, and Vince was the first storm in recorded history to reach the Iberian Peninsula as a tropical cyclone, i.e. Northeastern Atlantic Ocean: In October 2005, Hurricane Vince formed near Madeira, then moved northeastward, passing south of the Portuguese south coast, and made landfall in southwestern Spain as a tropical depression. However, there is debate on whether these storms were tropical in nature. Such cyclones formed in September 1947, September 1969, January 1982, September 1983, and January 1995.

    Mediterranean Sea: Storms which appear similar to tropical cyclones in structure sometimes occur in the Mediterranean basin. They affect the islands of Polynesia in exceptional instances. Most of the storms that enter this region formed farther west in the Southwest Pacific. Eastern South Pacific: Tropical cyclone formation is rare in this region; when they do form, it is frequently linked to El Niño episodes.

    However, this region is commonly frequented by tropical cyclones that form in the much more favorable Eastern North Pacific Basin. Central North Pacific: Shear in this area of the Pacific Ocean severely limits tropical development. The January storm is thought to have reached tropical storm intensity based on scatterometre winds. However, three tropical cyclones have been observed here — a weak tropical storm in 1991 off the coast of Africa, Hurricane Catarina (sometimes also referred to as Aldonça), which made landfall in Brazil in 2004 as a Category 1 hurricane, and a smaller storm in January 2004, east of Salvador, Brazil.

    Southern Atlantic Ocean: A combination of cooler waters, the lack of an ITCZ, and wind shear makes it very difficult for the Southern Atlantic to support tropical activity. Cyclones forming here impact Madagascar, Mozambique, Mauritius, and Kenya, and these nations issue forecasts and warnings for the basin. Southwestern Indian Ocean: This basin is the least understood, due to a lack of historical data. Southeastern Indian Ocean: Tropical activity in this region affects Australia and Indonesia, and is forecast by those nations.

    Rarely, a tropical cyclone formed in this basin will affect the Arabian Peninsula. Nations affected by this basin include India, Bangladesh, Sri Lanka, Thailand, Myanmar, and Pakistan, and all of these countries issue regional forecasts and warnings. Hurricanes which form in this basin have historically cost the most lives — most notably, the 1970 Bhola cyclone killed 200,000. This basin's season has an interesting double peak; one in April and May before the onset of the monsoon, and another in October and November just after.

    Northern Indian Ocean: This basin is divided into two areas, the Bay of Bengal and the Arabian Sea, with the Bay of Bengal dominating (5 to 6 times more activity). South Western Pacific Ocean: Tropical activity in this region largely affects Australia and Oceania, and is forecast by Australia and Papua New Guinea. In the U.S., the Central Pacific Hurricane Center is responsible for forecasting the western part of this area while the National Hurricane Center is responsible for the eastern part. Storms that form here can affect western Mexico, Hawaii, northern Central America, and on extremely rare occasions, California.

    Eastern North Pacific Ocean: This is the second most active basin in the world, and the most dense (a large number of storms for a small area of ocean). National meteorology organizations and the Joint Typhoon Warning Center (JTWC) are responsible for issuing forecasts and warnings in this basin. The eastern coasts of Taiwan and Philippines also have the highest tropical cyclone landfall frequency in the world. This is by far the most active basin, accounting for one-third of all tropical cyclone activity in the world.

    Western North Pacific Ocean: Tropical storm activity in this region frequently affects China, Japan, the Philippines, and Taiwan, but also many other countries in South-East Asia, such as Vietnam, South Korea and Indonesia, plus numerous Oceanian islands. Many of the more intense Atlantic storms are Cape Verde-type hurricanes, which form off the west coast of Africa near the Cape Verde islands. The coast of Atlantic Canada receives hurricane landfalls on rare occasion, such as Hurricane Juan in 2003. Gulf Coast and occasionally New Jersey, New York and New England (usually hurricanes weaken to tropical storms before they reach these northern regions).

    Additionally, they can hit the coast of the U.S., especially Florida, North Carolina, the U.S. Hurricanes that strike Mexico, Central America, and Caribbean island nations, often do intense damage, as hurricanes are deadlier over warmer water. National Hurricane Center (NHC) based in Miami, Florida, issues forecasts for storms for all nations in the region; the Canadian Hurricane Centre, based in Halifax, Nova Scotia, also issues forecasts and warnings for storms expected to affect Canadian territory and waters. The U.S.

    Venezuela, the south-east of Canada and Atlantic "Macaronesian" islands are also occasionally affected. The United States Atlantic coast, Mexico, Central America, the Caribbean Islands and Bermuda are frequently affected by storms in this basin. The average is about ten. Tropical cyclone formation here varies widely from year to year, ranging from over twenty to one per year.

    North Atlantic Basin: The most-studied of all tropical basins, it includes the Atlantic Ocean, the Caribbean Sea, and the Gulf of Mexico. If a low level circulation forms under this convection, it may develop into a tropical cyclone. Decaying frontal boundaries may occasionally stall over warm waters and produce lines of active convection. A warm-core tropical cyclone may result when one of these (on occasion) works down to the lower levels and produces deep convection.

    Tropical upper tropospheric troughs, which are cold-core upper level lows. A similar phenomenon to tropical waves are West African disturbance lines, which are squally lines of convection that form over Africa and move into the Atlantic. Most tropical cyclones form from these. This often assists in the development of thunderstorms, which can develop into tropical cyclones.

    Tropical waves, or easterly waves, which, as mentioned above, are westward moving areas of convergent winds. High wind shear can break apart the vertical structure of a tropical cyclone. Low vertical wind shear (change in wind speed or direction over height). (2004's Hurricane Ivan was the strongest storm to form closer than 10 degrees from the equator; it started forming at 9.7 degrees north.).

    A distance of approximately 10 degrees or more from the equator, so that the Coriolis effect is strong enough to initiate the cyclone's rotation. This is most frequently provided by tropical waves—non-rotating areas of thunderstorms that move through tropical oceans. A pre-existing weather disturbance. Temperature in the atmosphere must decrease quickly with height, and the mid-troposphere must be relatively moist.

    Upper-atmosphere conditions conducive to thunderstorm formation. The moisture in the air above the warm water is the energy source for tropical cyclones. Sea surface temperatures above 26.5 degrees Celsius (79.7 degrees Fahrenheit) to at least a depth of 50 meters (164 feet). From Urdu, Persian or Arabic ţūfān (طوفان) < Greek tuphōn (Τυφών).

    The first record of the character 颱 appeared in 1685's edition of Summary of Taiwan 臺灣記略). (The Chinese term as 颱風 táifēng, and 台風 taifu in Japanese, has an independent origin traceable variously to 風颱, 風篩 or 風癡 hongthai, going back to Song 宋 (960-1278) and Yuan 元(1260-1341) dynasties. From the Chinese 大風 (daaih fūng (Cantonese); dà fēng (Mandarin)) which means "great wind". Cyclone (unofficially): South Atlantic Ocean.

    Tropical cyclone: Southwest Indian Ocean and the South Pacific east of 160°E. Severe cyclonic storm: North Indian Ocean. Severe tropical cyclone: Southwest Pacific west of 160°E and the southeast Indian Ocean east of 90°E. Typhoon: Northwest Pacific west of the dateline.

    Hurricane: Atlantic basin and North Pacific Ocean east of the dateline.

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