A tropical wave (also called easterly wave , tropical easterly wave , and African easterly wave ), in and around the Atlantic Ocean , is a type of atmospheric trough , an elongated area of relatively low air pressure , oriented north to south, which moves from east to west across the tropics , causing areas of cloudiness and thunderstorms . Tropical waves form in the easterly flow along the equatorial side of the subtropical ridge or belt of high air pressure which lies north and south of the Intertropical Convergence Zone (ITCZ). Tropical waves are generally carried westward by the prevailing easterly winds along the tropics and subtropics near the equator . They can lead to the formation of tropical cyclones in the north Atlantic and northeastern Pacific basins . A tropical wave study is aided by Hovmöller diagrams , a graph of meteorological data.
131-746: Effects Other wikis Hurricane Mitch was the second-deadliest tropical cyclone in the Atlantic basin on record. Mitch caused 11,374 fatalities in Central America in 1998, including approximately 7,000 in Honduras and 3,800 in Nicaragua due to cataclysmic flooding from the slow motion of the storm. It was the deadliest hurricane in Central American history, surpassing Hurricane Fifi–Orlene , which killed slightly fewer people in
262-531: A Tropical Cyclone Warning Centre by the World Meteorological Organization 's (WMO) tropical cyclone programme. These warning centers issue advisories which provide basic information and cover a systems present, forecast position, movement and intensity, in their designated areas of responsibility. Meteorological services around the world are generally responsible for issuing warnings for their own country. There are exceptions, as
393-416: A 1.5 degree warming lead to "increased proportion of and peak wind speeds of intense tropical cyclones". We can say with medium confidence that regional impacts of further warming include more intense tropical cyclones and/or extratropical storms. Climate change can affect tropical cyclones in a variety of ways: an intensification of rainfall and wind speed, a decrease in overall frequency, an increase in
524-444: A 2019 review paper show a future increase of rainfall rates. Additional sea level rise will increase storm surge levels. It is plausible that extreme wind waves see an increase as a consequence of changes in tropical cyclones, further exacerbating storm surge dangers to coastal communities. The compounding effects from floods, storm surge, and terrestrial flooding (rivers) are projected to increase due to global warming . There
655-613: A circle, whirling round their central clear eye , with their surface winds blowing counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere . The opposite direction of circulation is due to the Coriolis effect . Tropical cyclones tend to develop during the summer, but have been noted in nearly every month in most tropical cyclone basins . Tropical cyclones on either side of
786-493: A final landfall near Naples, Florida on November 5. Shortly after crossing the state, Mitch transitioned into an extratropical cyclone . The NHC tracked this storm until November 9, when former Hurricane Mitch passed north of Scotland . Due to the threat, the government of Honduras evacuated some of the 45,000 citizens on the Bay Islands and prepared all air and naval resources. The government of Belize issued
917-405: A flow of warm, moist, rapidly rising air, which starts to rotate cyclonically as it interacts with the rotation of the earth. Several factors are required for these thunderstorms to develop further, including sea surface temperatures of around 27 °C (81 °F) and low vertical wind shear surrounding the system, atmospheric instability, high humidity in the lower to middle levels of
1048-506: A higher intensity. Most tropical cyclones that experience rapid intensification are traversing regions of high ocean heat content rather than lower values. High ocean heat content values can help to offset the oceanic cooling caused by the passage of a tropical cyclone, limiting the effect this cooling has on the storm. Faster-moving systems are able to intensify to higher intensities with lower ocean heat content values. Slower-moving systems require higher values of ocean heat content to achieve
1179-494: A hurricane on October 24 and developed an eye . After turning to the west, Mitch rapidly intensified , first into a major hurricane on October 25 and then into a Category 5 on the Saffir-Simpson Hurricane Scale the next day. At peak intensity, Mitch maintained maximum sustained winds of 180 mph (290 km/h) while off the northern coast of Honduras. Hurricane Hunters reported
1310-464: A large number of forecasting centers, uses infrared geostationary satellite imagery and an algorithm based upon the Dvorak technique to assess the intensity of tropical cyclones. The ADT has a number of differences from the conventional Dvorak technique, including changes to intensity constraint rules and the usage of microwave imagery to base a system's intensity upon its internal structure, which prevents
1441-464: A large role in both the classification of a tropical cyclone and the determination of its intensity. Used in warning centers, the method was developed by Vernon Dvorak in the 1970s, and uses both visible and infrared satellite imagery in the assessment of tropical cyclone intensity. The Dvorak technique uses a scale of "T-numbers", scaling in increments of 0.5 from T1.0 to T8.0. Each T-number has an intensity assigned to it, with larger T-numbers indicating
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#17327719580311572-551: A minimum barometric pressure of 905 mbar (26.7 inHg), which at the time was the lowest in the month of October and tied for the fourth lowest for any Atlantic hurricane . Initially, the National Hurricane Center (NHC) and various tropical cyclone forecast models anticipated a turn to the north, threatening the Yucatán Peninsula . Instead, Mitch turned to the south, due to a ridge that
1703-426: A much smaller area. This replenishing of moisture-bearing air after rain may cause multi-hour or multi-day extremely heavy rain up to 40 km (25 mi) from the coastline, far beyond the amount of water that the local atmosphere holds at any one time. This in turn can lead to river flooding , overland flooding, and a general overwhelming of local water control structures across a large area. A tropical cyclone
1834-438: A new, structurally improved foundation, homes were redesigned to be able to withstand another hurricane. However, lack of arable crop land took away the jobs from many, decreasing an already low income even lower. Following the passage of Mitch, disease outbreaks occurred throughout Central America, including cholera , leptospirosis , and dengue fever . Over 2,328 cases of cholera were reported, killing 34 people. Guatemala
1965-493: A number of techniques considered to try to artificially modify tropical cyclones. These techniques have included using nuclear weapons , cooling the ocean with icebergs, blowing the storm away from land with giant fans, and seeding selected storms with dry ice or silver iodide . These techniques, however, fail to appreciate the duration, intensity, power or size of tropical cyclones. A variety of methods or techniques, including surface, satellite, and aerial, are used to assess
2096-422: A process known as rapid intensification, a period in which the maximum sustained winds of a tropical cyclone increase by 30 kn (56 km/h; 35 mph) or more within 24 hours. Similarly, rapid deepening in tropical cyclones is defined as a minimum sea surface pressure decrease of 1.75 hPa (0.052 inHg) per hour or 42 hPa (1.2 inHg) within a 24-hour period; explosive deepening occurs when
2227-442: A purple alert and asked for citizens on offshore islands to leave for the mainland. Because the hurricane threatened to strike near Belize City as a Category 4 hurricane, much of the city was evacuated in fear of a repeat of Hurricane Hattie 37 years earlier. Guatemala issued a purple alert as well, recommending boats to stay in port, telling people to prepare or seek shelter, and warning of potential overflowing rivers. By
2358-429: A remnant low-pressure area . Remnant systems may persist for several days before losing their identity. This dissipation mechanism is most common in the eastern North Pacific. Weakening or dissipation can also occur if a storm experiences vertical wind shear which causes the convection and heat engine to move away from the center. This normally ceases the development of a tropical cyclone. In addition, its interaction with
2489-442: A result of the extreme damage and loss of life caused by Hurricane Mitch, the name Mitch was retired by the World Meteorological Organization following this storm, and will never again be used for a North Atlantic tropical cyclone. It was replaced with Matthew for the 2004 season . After the disaster, countries around the world donated significant aid, totaling $ 6.3 billion (1998 USD). Throughout Central America, which
2620-461: A shock to residents, and president Carlos Roberto Flores alike. The U.S. later increased their offer to $ 70 million (1998 USD). The Honduran government distributed food, water, and medical services to the hurricane victims, including the more than 4 million without water. In addition, the country initially experienced a sharp increase in the unemployment rate, largely due to the destruction of crop lands. However, rebuilding provided jobs in
2751-526: A spiral arrangement of thunderstorms that produce heavy rain and squalls . Depending on its location and strength, a tropical cyclone is called a hurricane ( / ˈ h ʌr ɪ k ən , - k eɪ n / ), typhoon ( / t aɪ ˈ f uː n / ), tropical storm , cyclonic storm , tropical depression , or simply cyclone . A hurricane is a strong tropical cyclone that occurs in the Atlantic Ocean or northeastern Pacific Ocean . A typhoon occurs in
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#17327719580312882-569: A storm. Tropical cyclone scales , such as the Saffir-Simpson hurricane wind scale and Australia's scale (Bureau of Meteorology), only use wind speed for determining the category of a storm. The most intense storm on record is Typhoon Tip in the northwestern Pacific Ocean in 1979, which reached a minimum pressure of 870 hPa (26 inHg ) and maximum sustained wind speeds of 165 kn (85 m/s; 305 km/h; 190 mph). The highest maximum sustained wind speed ever recorded
3013-581: A stronger system. Tropical cyclones are assessed by forecasters according to an array of patterns, including curved banding features , shear, central dense overcast, and eye, to determine the T-number and thus assess the intensity of the storm. The Cooperative Institute for Meteorological Satellite Studies works to develop and improve automated satellite methods, such as the Advanced Dvorak Technique (ADT) and SATCON. The ADT, used by
3144-405: A system has dissipated or lost its tropical characteristics, its remnants could regenerate a tropical cyclone if environmental conditions become favorable. A tropical cyclone can dissipate when it moves over waters significantly cooler than 26.5 °C (79.7 °F). This will deprive the storm of such tropical characteristics as a warm core with thunderstorms near the center, so that it becomes
3275-481: A temporary dam. Throughout the country, there were at least 7,000 fatalities, some reported in each department . Following the storm, officials in Honduras requested international assistance, which totaled $ 2.8 billion over a several-year period. Despite this, the gross domestic product began decreasing at the end of 1998, and contracted by 1.9 percent in 1999. Officials enacted a widespread curfew following
3406-529: A tropical cyclone are a result of the conservation of angular momentum imparted by the Earth's rotation as air flows inwards toward the axis of rotation. As a result, cyclones rarely form within 5° of the equator . Tropical cyclones are very rare in the South Atlantic (although occasional examples do occur ) due to consistently strong wind shear and a weak Intertropical Convergence Zone . In contrast,
3537-461: A tropical cyclone's core has a negative effect on its development and intensity by diminishing atmospheric convection and introducing asymmetries in the storm's structure. Symmetric, strong outflow leads to a faster rate of intensification than observed in other systems by mitigating local wind shear. Weakening outflow is associated with the weakening of rainbands within a tropical cyclone. Tropical cyclones may still intensify, even rapidly, in
3668-401: A tropical cyclone's intensity or the direction it is traveling. Wind-pressure relationships (WPRs) are used as a way to determine the pressure of a storm based on its wind speed. Several different methods and equations have been proposed to calculate WPRs. Tropical cyclones agencies each use their own, fixed WPR, which can result in inaccuracies between agencies that are issuing estimates on
3799-505: A tropical wave, leaving cloudless skies, as convection is capped by the dry layer inversion. Additionally, any dust in the SAL reflects sunlight, cooling the air below it. Tropical waves in the Atlantic basin develop from low-pressure disturbances, which develop as far east as Sudan in east Africa , and drift across the continent into the Atlantic Ocean . These are generated or enhanced by
3930-418: A tropical wave. This normally occurs if upper-level wind shear is too strong. The storm can redevelop if the upper-level shear abates. If a tropical wave is moving quickly, or is organized enough, it can have winds of a strength in excess of tropical storm force, but it is not considered a tropical storm unless it has a closed low-level circulation. An example of this was Hurricane Claudette in 2003 , where
4061-480: A two-digit number and suffix letter by the warning centers that monitor them. Tropical wave West-moving waves can also form from the tail end of frontal zones in the subtropics and tropics, and may be referred to as easterly waves, but the waves are not properly called tropical waves. They are a form of inverted trough that shares many characteristics of a tropical wave. A tropical wave normally follows an area of sinking, intensely dry air, blowing from
Hurricane Mitch - Misplaced Pages Continue
4192-831: A typhoon. This happened in 2014 for Hurricane Genevieve , which became Typhoon Genevieve. Within the Southern Hemisphere, it is either called a hurricane, tropical cyclone or a severe tropical cyclone, depending on if it is located within the South Atlantic, South-West Indian Ocean, Australian region or the South Pacific Ocean. The descriptors for tropical cyclones with wind speeds below 65 kn (120 km/h; 75 mph) vary by tropical cyclone basin and may be further subdivided into categories such as "tropical storm", "cyclonic storm", "tropical depression", or "deep depression". The practice of using given names to identify tropical cyclones dates back to
4323-415: Is assumed at this stage that a tropical cyclone has become self-sustaining and can continue to intensify without any help from its environment. Depending on its location and strength, a tropical cyclone is referred to by different names , including hurricane , typhoon , tropical storm , cyclonic storm , tropical depression , or simply cyclone . A hurricane is a strong tropical cyclone that occurs in
4454-406: Is calculated as: where p {\textstyle p} is the density of air, u {\textstyle u} is a sustained surface wind speed value, and d v {\textstyle d_{v}} is the volume element . Around the world, tropical cyclones are classified in different ways, based on the location ( tropical cyclone basins ), the structure of
4585-554: Is currently no consensus on how climate change will affect the overall frequency of tropical cyclones. A majority of climate models show a decreased frequency in future projections. For instance, a 2020 paper comparing nine high-resolution climate models found robust decreases in frequency in the Southern Indian Ocean and the Southern Hemisphere more generally, while finding mixed signals for Northern Hemisphere tropical cyclones. Observations have shown little change in
4716-414: Is cut off from its supply of warm moist maritime air and starts to draw in dry continental air. This, combined with the increased friction over land areas, leads to the weakening and dissipation of the tropical cyclone. Over a mountainous terrain, a system can quickly weaken. Over flat areas, it may endure for two to three days before circulation breaks down and dissipates. Over the years, there have been
4847-445: Is the generic term for a warm-cored, non-frontal synoptic-scale low-pressure system over tropical or subtropical waters around the world. The systems generally have a well-defined center which is surrounded by deep atmospheric convection and a closed wind circulation at the surface. A tropical cyclone is generally deemed to have formed once mean surface winds in excess of 35 kn (65 km/h; 40 mph) are observed. It
4978-512: Is the greatest. However, each particular basin has its own seasonal patterns. On a worldwide scale, May is the least active month, while September is the most active month. November is the only month in which all the tropical cyclone basins are in season. In the Northern Atlantic Ocean , a distinct cyclone season occurs from June 1 to November 30, sharply peaking from late August through September. The statistical peak of
5109-405: Is the storm's wind speed and r {\textstyle r} is the radius of hurricane-force winds. The Hurricane Severity Index is a scale that can assign up to 50 points to a system; up to 25 points come from intensity, while the other 25 come from the size of the storm's wind field. The IKE model measures the destructive capability of a tropical cyclone via winds, waves, and surge. It
5240-674: The African Easterly Jet . The clockwise circulation of the large transoceanic high-pressure cell or anticyclone centered near the Azores islands (known as the Azores High ) impels easterly waves away from the coastal areas of Africa towards North America . Tropical waves are the origin of approximately 60% of Atlantic tropical cyclones and of approximately 85% of intense Atlantic hurricanes ( Category 3 and greater). Tropical cyclones can sometimes degenerate back into
5371-620: The African easterly jet and areas of atmospheric instability give rise to cyclones in the Atlantic Ocean and Caribbean Sea . Heat energy from the ocean acts as the accelerator for tropical cyclones. This causes inland regions to suffer far less damage from cyclones than coastal regions, although the impacts of flooding are felt across the board. Coastal damage may be caused by strong winds and rain, high waves (due to winds), storm surges (due to wind and severe pressure changes), and
Hurricane Mitch - Misplaced Pages Continue
5502-573: The Atlantic Ocean or northeastern Pacific Ocean , and a typhoon occurs in the northwestern Pacific Ocean. In the Indian Ocean and South Pacific, comparable storms are referred to as "tropical cyclones", and such storms in the Indian Ocean can also be called "severe cyclonic storms". Tropical refers to the geographical origin of these systems, which form almost exclusively over tropical seas. Cyclone refers to their winds moving in
5633-413: The Bay Islands had damage to their water facilities. Two days of winds exceeding 200 km/h (125 mph) destroyed nearly all of the plants and trees on Guanaja, uprooting or knocking down almost the entire mangrove forest. It is estimated that the hurricane produced waves of 44 ft (13 m) in height. While moving slowly for several days offshore Honduras, Hurricane Mitch drew moisture from
5764-642: The Bay of Campeche . On November 3, the remnants redeveloped into a tropical storm just off the coast of the Mexican state of Campeche , and a day later the storm made another landfall just north of the city of Campeche . Mitch accelerated to the northeast ahead of a cold front , moving across the Yucatán peninsula and re-entering the Gulf of Mexico. The storm retained winds of 70 mph (110 km/h) before it made
5895-591: The Casita Volcano failed and turned into a lahar from excessive rain. The resulting mudslide ultimately covered an area 10 miles (16 km) long and 5 miles (8.0 km) wide. Two million people in Nicaragua were directly affected by the hurricane. Across the country, Mitch's heavy rains damaged 17,600 houses and destroyed 23,900, displacing 368,300 of the population. 340 schools and 90 health centers were severely damaged or destroyed. Sewage systems and
6026-647: The Hurricane Surge Index , the Hurricane Severity Index , the Power Dissipation Index (PDI), and integrated kinetic energy (IKE). ACE is a metric of the total energy a system has exerted over its lifespan. ACE is calculated by summing the squares of a cyclone's sustained wind speed, every six hours as long as the system is at or above tropical storm intensity and either tropical or subtropical. The calculation of
6157-476: The Isle of Youth and Cayo Largo del Sur to leave for safer grounds. In Jamaica , where officials declared hurricane warnings 12 hours prior to its closest approach, Mitch caused moderate rainfall and gusty winds for days. Strong waves hit western Jamaica, with wave heights unofficially estimated at nearly 7 feet (2.1 m) in height. The rainfall in outer rainbands, at times severe, flooded many roads across
6288-559: The Madden–Julian oscillation . The IPCC Sixth Assessment Report summarize the latest scientific findings about the impact of climate change on tropical cyclones. According to the report, we have now better understanding about the impact of climate change on tropical storm than before. Major tropical storms likely became more frequent in the last 40 years. We can say with high confidence that climate change increase rainfall during tropical cyclones. We can say with high confidence that
6419-460: The Saffir–Simpson scale . Climate oscillations such as El Niño–Southern Oscillation (ENSO) and the Madden–Julian oscillation modulate the timing and frequency of tropical cyclone development. Rossby waves can aid in the formation of a new tropical cyclone by disseminating the energy of an existing, mature storm. Kelvin waves can contribute to tropical cyclone formation by regulating
6550-575: The Saffir–Simpson scale . The trend was most clear in the North Atlantic and in the Southern Indian Ocean. In the North Pacific, tropical cyclones have been moving poleward into colder waters and there was no increase in intensity over this period. With 2 °C (3.6 °F) warming, a greater percentage (+13%) of tropical cyclones are expected to reach Category 4 and 5 strength. A 2019 study indicates that climate change has been driving
6681-641: The Yucatán Peninsula , with Cancún on the Quintana Roo coast being the worst hit. Nine people were killed from the flooding, though damage was relatively minimal. The maximum 24-hour rainfall total from Mitch was 13.4 inches (340 mm) in Campeche , while the highest rainfall total was 16.85 inches (428.0 mm) in Ciudad del Carmen . Mitch was also responsible for the loss with all hands of Windjammer Barefoot Cruises ' schooner Fantome . The story
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#17327719580316812-515: The fowl population. Crop and agricultural damage totaled about $ 1 billion, which would take the country years to recover. Honduras's Social Fund for Housing estimated that 35,000 houses nationwide were destroyed with another 50,000 damaged, leaving 1.5 million people homeless – about 20% of the total population. This was the highest number of victims from any natural disaster in Honduras's history. Overall, Hurricane Mitch killed about 7,000 people in Honduras, and damage
6943-504: The most disastrous impacts came from Honduras , which suffered over half of the total deaths. The president of Honduras, Carlos Roberto Flores , estimated that Mitch set back about 50 years of economic development. The storm wrecked about 35,000 houses and damaged another 50,000, leaving up to 1.5 million people homeless, about 20 percent of the country's population. Mitch directly caused $ 2.005 billion in damage, with an additional $ 1.8 billion in indirect costs. Most of
7074-495: The northeast . After the passage of the trough line, the wind veers southeast, the humidity abruptly rises, and the atmosphere destabilizes . This yields widespread showers and thunderstorms , sometimes severe . As the wave moves westward, the showers gradually diminish. An exception to the association of convection can occur in the Atlantic. Sometimes, a surge of dry air called the Saharan Air Layer (SAL) follows
7205-514: The troposphere , enough Coriolis force to develop a low-pressure center , and a pre-existing low-level focus or disturbance. There is a limit on tropical cyclone intensity which is strongly related to the water temperatures along its path. and upper-level divergence. An average of 86 tropical cyclones of tropical storm intensity form annually worldwide. Of those, 47 reach strength higher than 119 km/h (74 mph), and 20 become intense tropical cyclones, of at least Category 3 intensity on
7336-584: The Atlantic hurricane season is September 10. The Northeast Pacific Ocean has a broader period of activity, but in a similar time frame to the Atlantic. The Northwest Pacific sees tropical cyclones year-round, with a minimum in February and March 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,
7467-498: The Caribbean estimated that Mitch caused the worst floods of the 20th century in the country. An estimated 70–80% of transportation network was destroyed, including most bridges and secondary roads, amounting to $ 236 million in damage. Hurricane Mitch left widespread power outages after damaging more than 385 km (239 mi) of power lines and several power plants. About 70% of Honduras lost access to fresh water after
7598-556: The Equator generally have their origins in the Intertropical Convergence Zone , where winds blow from either the northeast or southeast. Within this broad area of low-pressure, air is heated over the warm tropical ocean and rises in discrete parcels, which causes thundery showers to form. These showers dissipate quite quickly; however, they can group together into large clusters of thunderstorms. This creates
7729-632: The PDI is similar in nature to ACE, with the major difference being that wind speeds are cubed rather than squared. The Hurricane Surge Index is a metric of the potential damage a storm may inflict via storm surge. It is calculated by squaring the dividend of the storm's wind speed and a climatological value (33 m/s or 74 mph), and then multiplying that quantity by the dividend of the radius of hurricane-force winds and its climatological value (96.6 km or 60.0 mi). This can be represented in equation form as: where v {\textstyle v}
7860-734: The Pacific Ocean and the Caribbean Sea, producing high amounts of rainfall of over 300 mm (12 in) per day. The highest official total was 928 mm (36.5 in) at Choluteca , which represented more than half of the annual precipitation average; at the same location, 466.7 mm (18.37 in) fell in a 24-hour period on October 31, which was more than double of the previous record set in 1985. There were unofficial rainfall totals in Central America as high as 1,900 mm (75 in); rain gauges in mountainous areas were washed away. The high rainfall caused many rivers in
7991-463: The South Atlantic is not a major basin, and not an official basin according to the WMO. Each year on average, around 80 to 90 named tropical cyclones form around the world, of which over half develop hurricane-force winds of 65 kn (120 km/h; 75 mph) or more. Worldwide, tropical cyclone activity peaks in late summer, when the difference between temperatures aloft and sea surface temperatures
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#17327719580318122-592: The United Kingdom. In Ireland, the storm produced gusts as high as 90 mph (140 km/h) and 30 ft (9.1 m) waves. The winds knocked down trees and power lines, leaving over 30,000 homes without power. One tree fell onto a car in Louth , severely injuring the driver. In Dublin , high winds knocked the roof off of a building, and several other buildings nationwide were damaged. The storm caused airports to close and ferry service to be suspended. As
8253-610: The United States National Hurricane Center and Fiji Meteorological Service issue alerts, watches and warnings for various island nations in their areas of responsibility. The United States Joint Typhoon Warning Center and Fleet Weather Center also publicly issue warnings about tropical cyclones on behalf of the United States Government . The Brazilian Navy Hydrographic Center names South Atlantic tropical cyclones , however
8384-591: The Western Pacific. Tropical cyclones have to have a significant amount of gale-force winds occurring around the center before they are named within the Southern Hemisphere . The names of significant tropical cyclones in the North Atlantic Ocean, Pacific Ocean, and Australian region are retired from the naming lists and replaced with another name. Tropical cyclones that develop around the world are assigned an identification code consisting of
8515-446: The bean production, 19% of the corn production, and 20% losses in sugar canes. There were heavy losses in livestock as well, including the deaths of 10,000 cattle. Total agricultural and livestock damaged amounted to $ 154 million (1998 USD). In addition, the flooding destroyed two bridges and damaged 1,200 mi (1,900 km) of unpaved roads. In all, Mitch caused nearly $ 400 million in damage (1998 USD) and 240 deaths. Similar to
8646-404: The coral. However, the hurricane's upwelling cooled the warm water temperatures, preventing significant bleaching and destruction of the coral reef. Mitch caused such massive and widespread damage that Carlos Roberto Flores , the president of Honduras , claimed it destroyed fifty years of progress in the country. Honduras, the country most affected by the hurricane, received significant aid for
8777-611: The country to overflow "to an unprecedented extent this century", as described by the United Nations. The rainfall collected in rivers, causing extensive river flooding across the country. The greatest depth recorded was 12.5 m (41 ft) on the Ulúa River near Chinda , whilst the greatest width recorded was 359 m (1,178 ft) on the Río Lean near Arizona . The rainfall also caused widespread mudslides across
8908-689: The country, mostly in the northeastern part of the country. The storm impacted 2,135 homes to some degree, of which 241 were destroyed, leaving 4,000 homeless. Throughout the country, the rainfall and mudslides affected 126 bridges and 800 miles (1,300 km) or roads, mostly on the Inter-American Highway which was affected by Hurricane Cesar , two years prior. Mitch affected 115 sq mi (300 km) of crop lands, causing damage to both export and domestic crops. In all, Hurricane Mitch caused $ 92 million in damage (1998 USD) and seven deaths. While drifting through El Salvador ,
9039-409: The damage were ruined crops, and cash crop exports were cut by 9.4 percent in 1999, largely due to the storm. Over 70 percent of the transportation infrastructure was damaged, mostly damaged highways and bridges. Widespread areas experienced power outages, and about 70 percent of the country lost its water sources after the storm. In Tegucigalpa , a large landslide affected three neighborhoods and formed
9170-435: The development of the westerlies . Cyclone formation is usually reduced 3 days prior to the wave's crest and increased during the 3 days after. The majority of tropical cyclones each year form in one of seven tropical cyclone basins, which are monitored by a variety of meteorological services and warning centers. Ten of these warning centers worldwide are designated as either a Regional Specialized Meteorological Centre or
9301-408: The electricity subsector were severely damaged, and, combined with property, damage totaled to $ 300 million (1998 USD). Transportation was greatly affected by the hurricane, as well. The rainfall left 70% of the roads unusable or destroyed and greatly damaged 92 bridges. Over 1,700 miles (2,700 km) of highways or access roads needed replacement subsequent to the storm, especially in
9432-675: The entire country, the hurricane left between 500,000 and 800,000 homeless. In all, damage in Nicaragua is estimated at $ 1 billion (1998 USD). Due to Mitch's large circulation, it dropped heavy precipitation as far south as Panama and Colombia , especially in the Darién and Chiriquí provinces. The flooding washed away a few roads and bridges, and damaged numerous houses and schools, leaving thousands homeless. The hurricane left three casualties in Panama. In Costa Rica , Mitch dropped heavy rains, causing flash flooding and mudslides across
9563-492: The equator, then move poleward past the ridge axis before recurving into the main belt of the Westerlies . When the subtropical ridge position shifts due to El Niño, so will the preferred tropical cyclone tracks. Areas west of Japan and Korea tend to experience much fewer September–November tropical cyclone impacts during El Niño and neutral years. During La Niña years, the formation of tropical cyclones, along with
9694-469: The evaporation of water from the ocean surface, which ultimately condenses into clouds and rain when moist air rises and cools to saturation . This energy source differs from that of mid-latitude cyclonic storms , such as nor'easters and European windstorms , which are powered primarily by horizontal temperature contrasts . Tropical cyclones are typically between 100 and 2,000 km (62 and 1,243 mi) in diameter. The strong rotating winds of
9825-481: The eyewall of the storm, and an upper-level anticyclone helps channel this air away from the cyclone efficiently. However, some cyclones such as Hurricane Epsilon have rapidly intensified despite relatively unfavorable conditions. There are a number of ways a tropical cyclone can weaken, dissipate, or lose its tropical characteristics. These include making landfall, moving over cooler water, encountering dry air, or interacting with other weather systems; however, once
9956-407: The following years. In Costa Rica , reconstruction after the hurricane increased the number of jobs by 5.9%, lowering the unemployment rate slightly. [REDACTED] Media related to Hurricane Mitch at Wikimedia Commons Tropical cyclone A tropical cyclone is a rapidly rotating storm system with a low-pressure center, a closed low-level atmospheric circulation , strong winds, and
10087-410: The form of cold water from falling raindrops (this is because the atmosphere is cooler at higher altitudes). Cloud cover may also play a role in cooling the ocean, by shielding the ocean surface from direct sunlight before and slightly after the storm passage. All these effects can combine to produce a dramatic drop in sea surface temperature over a large area in just a few days. Conversely, the mixing of
10218-453: The frequency of very intense storms and a poleward extension of where the cyclones reach maximum intensity are among the possible consequences of human-induced climate change. Tropical cyclones use warm, moist air as their fuel. As climate change is warming ocean temperatures , there is potentially more of this fuel available. Between 1979 and 2017, there was a global increase in the proportion of tropical cyclones of Category 3 and higher on
10349-532: The general public regarding forecasts, watches, and warnings. Since the systems can last a week or longer, and more than one can be occurring in the same basin at the same time, the names are thought to reduce the confusion about what storm is being described. Names are assigned in order from predetermined lists with one, three, or ten-minute sustained wind speeds of more than 65 km/h (40 mph) depending on which basin it originates. Standards vary from basin to basin. Some tropical depressions are named in
10480-424: The highest possible rating on the Saffir–Simpson scale . After drifting southwestward and weakening, the hurricane hit Honduras as a minimal Category 1 hurricane. Mitch roved through Central America, regenerated in the Bay of Campeche , and ultimately impacted Florida as a strong tropical storm. It then became extratropical and accelerated northeastward across the North Atlantic, before dissipating on 9 November. At
10611-440: The hurricane caused strong waves, gusty winds, and heavy rainfall at times. Damage was relatively minimal, amounting to blown out windows and beach erosion . Strong waves damaged or destroyed many docks on the south shore of the islands, and also sank one dive ship near Grand Cayman . In addition, numerous incoming and outgoing flights were cancelled. Then a tropical storm, Mitch caused a storm surge of up to 4 feet (1.2 m) in
10742-619: The hurricane dropped immense amounts of precipitation, resulting in flash flooding and mudslides through the country. Multiple rivers, including the Río Grande de San Miguel and the Lempa River overflowed, contributing to overall damage. The flooding damaged more than 10,000 houses, leaving around 84,000 homeless and forcing 500,000 to evacuate. Crop damage was severe, with serious flooding occurring on 386 sq mi (1,000 km) of pasture or crop land. The flooding destroyed 37% of
10873-417: The hurricane was less severe than initially predicted, though Mitch still caused heavy rainfall across the country. Numerous rivers exceeded their crests, though the rainfall was beneficial to trees in mountainous areas. The flooding caused extensive crop damage and destroyed many roads. Throughout the country, eleven people died because of the hurricane. In Mexico, Mitch produced gusty winds and heavy rains on
11004-451: The intensity from leveling off before an eye emerges in infrared imagery. The SATCON weights estimates from various satellite-based systems and microwave sounders , accounting for the strengths and flaws in each individual estimate, to produce a consensus estimate of a tropical cyclone's intensity which can be more reliable than the Dvorak technique at times. Multiple intensity metrics are used, including accumulated cyclone energy (ACE),
11135-522: The intensity of a tropical cyclone. Reconnaissance aircraft fly around and through tropical cyclones, outfitted with specialized instruments, to collect information that can be used to ascertain the winds and pressure of a system. Tropical cyclones possess winds of different speeds at different heights. Winds recorded at flight level can be converted to find the wind speeds at the surface. Surface observations, such as ship reports, land stations, mesonets , coastal stations, and buoys, can provide information on
11266-538: The island and left them covered with debris. One house in Spanish Town collapsed from the flooding, leaving four homeless. Many other homes and buildings were flooded, forcing many to evacuate. A river in northeastern Jamaica overflowed its banks, while heavy rainfall across the mountainous parts of the country caused numerous mudslides. In all, Mitch killed three people on Jamaica. On the Cayman Islands ,
11397-693: The late 1800s and early 1900s and gradually superseded the existing system—simply naming cyclones based on what they hit. The system currently used provides positive identification of severe weather systems in a brief form, that is readily understood and recognized by the public. The credit for the first usage of personal names for weather systems is generally given to the Queensland Government Meteorologist Clement Wragge who named systems between 1887 and 1907. This system of naming weather systems fell into disuse for several years after Wragge retired, until it
11528-742: The lower Florida Keys before making landfall on the Florida west coast. Key West International Airport reported peak wind gusts of 55 mph (89 km/h) and sustained winds of 40 mph (64 km/h), the only report of tropical storm force in the state. Offshore, the Fowey Rocks Light reported wind gusts of 73 mph (117 km/h). In addition, Mitch caused moderate rainfall, peaking at 7 inches (200 mm) in Jupiter , though some estimates indicate localized totals of up to 10 inches (250 mm). The storm spawned five tornadoes over
11659-404: The main belt of the Westerlies , by means of merging with a nearby frontal zone, can cause tropical cyclones to evolve into extratropical cyclones . This transition can take 1–3 days. Should a tropical cyclone make landfall or pass over an island, its circulation could start to break down, especially if it encounters mountainous terrain. When a system makes landfall on a large landmass, it
11790-467: The millions impacted by the hurricane. Mexico quickly gave help, sending 700 tons of food, 11 tons of medicine, four rescue planes, rescue personnel, and trained search dogs. Cuba also volunteered, sending a contingent of physicians to the country. The U.S. administration offered at first troops stationed in Honduras, and then withdrew them a few days after the storm. They also at first offered only $ 2 million (1998 USD) in aid, which came as
11921-530: The mountainous country. In the country's interior, particularly the southern portion, the high rainfall caused hundreds of landslides , many of them shallow and about 95% in the form of debris flow . However, two earthflows caused significant damage near Tegucigalpa. Hurricane Mitch wrought significant damage to Honduras, affecting nearly the entire population and causing damage in all 18 departments . The United Nations Economic Commission for Latin America and
12052-482: The northern part of the country and along portions of the Pan-American Highway . Total transportation damage amounted to $ 300 million (1998 USD). Agricultural losses were significant, including the deaths of 50,000 animals, mostly bovines. Crops and fisheries were affected greatly as well, and, combined with agricultural losses, damage totaled to $ 185 million (1998 USD). The situation
12183-453: The northwestern Pacific Ocean. In the Indian Ocean and South Pacific, comparable storms are referred to as "tropical cyclones". In modern times, on average around 80 to 90 named tropical cyclones form each year around the world, over half of which develop hurricane-force winds of 65 kn (120 km/h; 75 mph) or more. Tropical cyclones typically form over large bodies of relatively warm water. They derive their energy through
12314-522: The observed trend of rapid intensification of tropical cyclones in the Atlantic basin. Rapidly intensifying cyclones are hard to forecast and therefore pose additional risk to coastal communities. Warmer air can hold more water vapor: the theoretical maximum water vapor content is given by the Clausius–Clapeyron relation , which yields ≈7% increase in water vapor in the atmosphere per 1 °C (1.8 °F) warming. All models that were assessed in
12445-549: The original wave had winds of 45 mph (72 km/h) before developing a closed low-level circulation. It has been suggested that some eastern Pacific Ocean tropical cyclones are formed out of tropical easterly waves that originate in North Africa as well. After developing into a tropical cyclone, some of those systems can then reach the Central Pacific Ocean, such as Hurricane Lane in 2018. During
12576-466: The overall frequency of tropical cyclones worldwide, with increased frequency in the North Atlantic and central Pacific, and significant decreases in the southern Indian Ocean and western North Pacific. There has been a poleward expansion of the latitude at which the maximum intensity of tropical cyclones occurs, which may be associated with climate change. In the North Pacific, there may also have been an eastward expansion. Between 1949 and 2016, there
12707-440: The potential of spawning tornadoes . Climate change affects tropical cyclones in several ways. Scientists found that climate change can exacerbate the impact of tropical cyclones by increasing their duration, occurrence, and intensity due to the warming of ocean waters and intensification of the water cycle . Tropical cyclones draw in air from a large area and concentrate the water content of that air into precipitation over
12838-413: The presence of moderate or strong wind shear depending on the evolution and structure of the storm's convection. The size of tropical cyclones plays a role in how quickly they intensify. Smaller tropical cyclones are more prone to rapid intensification than larger ones. The Fujiwhara effect , which involves interaction between two tropical cyclones, can weaken and ultimately result in the dissipation of
12969-444: The release of latent heat from the saturated soil. Orographic lift can cause a significant increase in the intensity of the convection of a tropical cyclone when its eye moves over a mountain, breaking the capped boundary layer that had been restraining it. Jet streams can both enhance and inhibit tropical cyclone intensity by influencing the storm's outflow as well as vertical wind shear. On occasion, tropical cyclones may undergo
13100-803: The rest of Central America, Mitch's heavy rains caused mudslides and severe flooding over Guatemala . The flooding destroyed 6,000 houses and damaged 20,000 others, displacing over 730,000 and forcing over 100,000 to evacuate. In addition, the flooding destroyed 27 schools and damaged 286 others, 175 severely. Flooding caused major damage to crops, while landslides destroyed crop land across the country. The most severely affected crops for domestic consumption were tomatoes, bananas, corn, other vegetables, and beans, with damaged totaling to $ 48 million (1998 USD). Export crops such as bananas or coffee were greatly damaged as well, with damage amounting to $ 325 million (1998 USD). Damage to plantations and soil totaled to $ 121 million (1998 USD). The flooding also caused severe damage to
13231-572: The same area in 1974. Mitch was the deadliest Atlantic hurricane in the satellite era, and the second-deadliest on record in the Atlantic, only behind the Great Hurricane of 1780 which killed at least 22,000 people. The thirteenth named storm , ninth hurricane, and third major hurricane of the 1998 Atlantic hurricane season , Mitch formed in the western Caribbean Sea on 22 October, and after responding to extremely favorable conditions, it rapidly strengthened to peak at Category 5 status,
13362-492: The same intensity. The passage of a tropical cyclone over the ocean causes the upper layers of the ocean to cool substantially, a process known as upwelling , which can negatively influence subsequent cyclone development. This cooling is primarily caused by wind-driven mixing of cold water from deeper in the ocean with the warm surface waters. This effect results in a negative feedback process that can inhibit further development or lead to weakening. Additional cooling may come in
13493-492: The same system. The ASCAT is a scatterometer used by the MetOp satellites to map the wind field vectors of tropical cyclones. The SMAP uses an L-band radiometer channel to determine the wind speeds of tropical cyclones at the ocean surface, and has been shown to be reliable at higher intensities and under heavy rainfall conditions, unlike scatterometer-based and other radiometer-based instruments. The Dvorak technique plays
13624-513: The sea can result in heat being inserted in deeper waters, with potential effects on global climate . Vertical wind shear decreases tropical cyclone predicability, with storms exhibiting wide range of responses in the presence of shear. Wind shear often negatively affects tropical cyclone intensification by displacing moisture and heat from a system's center. Low levels of vertical wind shear are most optimal for strengthening, while stronger wind shear induces weakening. Dry air entraining into
13755-426: The second deadliest Atlantic hurricane in history after the Great Hurricane of 1780 ; at least 11,374 people were confirmed to have been killed with over 11,000 left missing by the end of 1998; the true death toll is unknown. Additionally, roughly 2.7 million were left homeless as a result of the hurricane. Total damages caused by the hurricane were estimated to be around $ 6 billion (1998 USD). The name "Mitch"
13886-600: The slow-moving hurricane and then tropical storm dropped nearly 36 inches (900 mm) of rain. The flooding and mudslides damaged or destroyed tens of thousands of homes, with total damage amounting to over $ 5 billion (1998 USD, $ 6 billion 2006 USD), most of which was in Honduras and Nicaragua . Prior to Mitch, the deadliest hurricane in Central America was Hurricane Fifi in 1974, which killed an estimated 8,000–10,000. While offshore northern Honduras, Hurricane Mitch passed over Guanaja island. High waves eroded northern coastlines and damaged lagoons. Most of
14017-595: The state, the strongest of which was rated F2 . In the Florida Keys, multiple buildings that had been damaged by Hurricane Georges were leveled by Mitch. Tornadoes from the storm damaged or destroyed 645 houses across the state, in addition to injuring 65 people. Gusty winds left 100,000 without power during the storm's passage. In all, Mitch caused $ 40 million in damage (1998 USD) in Florida and two deaths from drowning when two boats capsized. As an extratropical cyclone, Mitch passed west of Ireland and
14148-672: The storm, although many rural areas had already been experiencing water shortages. The combined damage to transportation, communication, utilities, including power and water, was estimated at $ 665 million. High water levels along the Choluteca River affected the capital, Tegucigalpa , reaching levels 10 m (33 ft) above their banks. The floods damaged about one-third of buildings, including some more than 350 years old. Across Honduras, agriculture sustained serious damage, with initial estimates of 70% of crops destroyed. About 50,000 bovine were killed, as were 60% of
14279-446: The storm, and for 15 days temporarily restricted constitutional rights to maintain order. There were outbreaks of various diseases, and many residents faced food and water shortages. Due to the slow motion from 29 October to 3 November, Hurricane Mitch dropped historic amounts of rainfall in Honduras , Guatemala , and Nicaragua , with unofficial reports of up to 75 inches (1,900 mm). Deaths due to catastrophic flooding made it
14410-617: The subtropical ridge position, shifts westward across the western Pacific Ocean, which increases the landfall threat to China and much greater intensity in the Philippines . The Atlantic Ocean experiences depressed activity due to increased vertical wind shear across the region during El Niño years. Tropical cyclones are further influenced by the Atlantic Meridional Mode , the Quasi-biennial oscillation and
14541-419: The summer months, tropical waves can extend northward as far as the desert of the southwestern United States, producing spells of intensified shower activity embedded within the prevailing monsoon regime. A screaming eagle is a tropical wave with a convective pattern that loosely resembles the head of an eagle. This phenomenon is caused by shearing from either westerly winds aloft or strong easterly winds at
14672-419: The surface pressure decreases by 2.5 hPa (0.074 inHg) per hour for at least 12 hours or 5 hPa (0.15 inHg) per hour for at least 6 hours. For rapid intensification to occur, several conditions must be in place. Water temperatures must be extremely high, near or above 30 °C (86 °F), and water of this temperature must be sufficiently deep such that waves do not upwell cooler waters to
14803-483: The surface. On the other hand, Tropical Cyclone Heat Potential is one of such non-conventional subsurface oceanographic parameters influencing the cyclone intensity. Wind shear must be low. When wind shear is high, the convection and circulation in the cyclone will be disrupted. Usually, an anticyclone in the upper layers of the troposphere above the storm must be present as well—for extremely low surface pressures to develop, air must be rising very rapidly in
14934-408: The surface. These systems are typically located within 25 degrees latitude of the equator. Rain showers and surface winds gusting to 29 mph (47 km/h) are associated with these waves. They move across the ocean at a rate of 15 mph (24 km/h). Strong thunderstorm activity can be associated with the features when located east of a tropical upper tropospheric trough . The term
15065-648: The system and its intensity. For example, within the Northern Atlantic and Eastern Pacific basins, a tropical cyclone with wind speeds of over 65 kn (120 km/h; 75 mph) is called a hurricane , while it is called a typhoon or a severe cyclonic storm within the Western Pacific or North Indian oceans. When a hurricane passes west across the International Dateline in the Northern Hemisphere, it becomes known as
15196-665: The time hurricane Mitch made landfall, numerous people were evacuated along the western Caribbean coastline, including 100,000 in Honduras, 10,000 in Guatemala, and 20,000 in the Mexican state of Quintana Roo . Hurricane Mitch was the deadliest Atlantic hurricane since the Great Hurricane of 1780 , displacing the Galveston Hurricane of 1900 as the second-deadliest on record. Nearly 11,000 people were confirmed dead, and almost as many reported missing. Deaths were mostly from flooding and mudslides in Central America, where
15327-417: The time, Mitch was the strongest Atlantic hurricane observed in the month of October, though it has since been surpassed by Hurricane Wilma of the 2005 season . In addition, Mitch is the ninth-most intense Atlantic hurricane on record, tied with Hurricane Dean in 2007 in terms of pressure. Being "the deadliest Atlantic hurricane" in over 200 years, Mitch caused catastrophic impacts across its path, but
15458-410: The transportation infrastructure, including the loss of 37 bridges. Across the country, flooding damaged or destroyed 840 miles (1,350 km) of roads, of which nearly 400 miles (640 km) were sections of major highways. In all, Hurricane Mitch caused $ 748 million (1998 USD) and 268 deaths in Guatemala. In addition, Mitch caused 11 indirect deaths when a plane crashed during the storm. In Belize ,
15589-423: The tropical cyclone year begins on July 1 and runs all year-round encompassing the tropical cyclone seasons, which run from November 1 until the end of April, with peaks in mid-February to early March. Of various modes of variability in the climate system, El Niño–Southern Oscillation has the largest effect on tropical cyclone activity. Most tropical cyclones form on the side of the subtropical ridge closer to
15720-451: The weaker of two tropical cyclones by reducing the organization of the system's convection and imparting horizontal wind shear. Tropical cyclones typically weaken while situated over a landmass because conditions are often unfavorable as a result of the lack of oceanic forcing. The Brown ocean effect can allow a tropical cyclone to maintain or increase its intensity following landfall , in cases where there has been copious rainfall, through
15851-402: The wind speed of Hurricane Helene by 11%, it increased the destruction from it by more than twice. According to World Weather Attribution the influence of climate change on the rainfall of some latest hurricanes can be described as follows: Tropical cyclone intensity is based on wind speeds and pressure. Relationships between winds and pressure are often used in determining the intensity of
15982-795: Was 185 kn (95 m/s; 345 km/h; 215 mph) in Hurricane Patricia in 2015—the most intense cyclone ever recorded in the Western Hemisphere . Warm sea surface temperatures are required for tropical cyclones to form and strengthen. The commonly-accepted minimum temperature range for this to occur is 26–27 °C (79–81 °F), however, multiple studies have proposed a lower minimum of 25.5 °C (77.9 °F). Higher sea surface temperatures result in faster intensification rates and sometimes even rapid intensification . High ocean heat content , also known as Tropical Cyclone Heat Potential , allows storms to achieve
16113-527: Was a slowdown in tropical cyclone translation speeds. It is unclear still to what extent this can be attributed to climate change: climate models do not all show this feature. A 2021 study review article concluded that the geographic range of tropical cyclones will probably expand poleward in response to climate warming of the Hadley circulation . When hurricane winds speed rise by 5%, its destructive power rise by about 50%. Therfore, as climate change increased
16244-477: Was estimated at L 52,345,000,000 ($ 3.8 billion), of which $ 2.005 billion was from direct damages and the remainder from indirect costs. The overall impact represented about 70% of Honduras's annual gross domestic product (GDP). Though Mitch never entered Nicaragua , its large circulation caused extensive rainfall, with estimates of over 50 inches (1,300 mm). In some places, as much as 25 inches (630 mm) of rain fell on coastal areas. The flank of
16375-586: Was further compounded by a total of 75,000 live land mines —left over from the Contra insurgency of the 1980s—that were calculated to have been uprooted and relocated by the floodwaters. In all, Hurricane Mitch caused at least 3,800 fatalities in Nicaragua, of which more than 2,000 were killed in the towns of El Provenir and Rolando Rodriguez from the landslide at the Casita volcano. The mudslide buried at least four villages completely in several feet of mud. Throughout
16506-521: Was most affected by the bacterium, where most of the deaths occurred from contaminated food. 450 cases of leptospirosis were reported in Nicaragua, killing seven people. There were over 1,357 cases of dengue reported, though no deaths were reported from the disease. While stalling over the western Caribbean Sea, Mitch's strong winds produced strong waves, damaging local coral reefs . Later, the storm's immense rainfall led to runoff polluted with debris and fresh water. This resulted in diseases occurring within
16637-419: Was not observed while the storm was active. Land interaction imparted weakening, and the hurricane made landfall on Honduras on October 29 with winds of 80 mph (130 km/h). While over land, Mitch moved slowly westward through Central America, while continuing to produce deep convection over waters. The surface circulation dissipated on November 1. The next day, the remnants of Mitch reached
16768-456: Was recorded in the book The Ship and The Storm by Jim Carrier. The schooner, which was sailing near the center of the hurricane, experienced over 50 feet (15 m) waves and over 100 mph (160 km/h) winds, causing her to sink off the coast of Honduras. On the south coast of Cuba , the hurricane caused waves of up to 13 feet (4.0 m) high and winds gusts peaking at 42 mph (68 km/h), causing numerous tourists and workers on
16899-401: Was recovering from an economic crisis that occurred in 1996, many wished to continue the growth of the infrastructure and economy. In addition, after witnessing the vulnerability to hurricanes, the affected governments endeavored to prevent such a disaster from occurring again. Hundreds of thousands of people lost their homes, but many took this as an opportunity to rebuild stronger houses. With
17030-584: Was retired, and will not be used for another Atlantic tropical cyclone. Tropical Depression Thirteen formed on October 22 over the southwestern Caribbean Sea, from a tropical wave that exited Africa on October 10. It executed a small loop, and while doing so intensified into Tropical Storm Mitch. A weakness in a ridge allowed the storm to track slowly to the north. After becoming disorganized due to wind shear from an upper-level low , Mitch quickly intensified in response to extremely favorable conditions, including warm waters and good outflow . It became
17161-585: Was revived in the latter part of World War II for the Western Pacific. Formal naming schemes have subsequently been introduced for the North and South Atlantic, Eastern, Central, Western and Southern Pacific basins as well as the Australian region and Indian Ocean. At present, tropical cyclones are officially named by one of twelve meteorological services and retain their names throughout their lifetimes to provide ease of communication between forecasters and
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