This article includes a list of references, but its sources remain unclear because it has insufficient inline citations . (October 2016) (Learn how and when to remove this template message)
States that border the Gulf of Mexico are shown in red.
|Principal cities|| Houston |
|Largest metropolitan area||Greater Houston|
The Gulf Coast of the United States is the coastline along the Southern United States where they meet the Gulf of Mexico. The coastal states that have a shoreline on the Gulf of Mexico are Texas, Louisiana, Mississippi, Alabama, and Florida, and these are known as the Gulf States.
The southern United States, also known as the American South, Dixie, Dixieland, or simply the South, is a region of the United States of America. It is located between the Atlantic Ocean and the western United States, with the midwestern United States and northeastern United States to its north and the Gulf of Mexico and Mexico to its south.
The Gulf of Mexico is an ocean basin and a marginal sea of the Atlantic Ocean, largely surrounded by the North American continent. It is bounded on the northeast, north and northwest by the Gulf Coast of the United States, on the southwest and south by Mexico, and on the southeast by Cuba. The U.S. states of Texas, Louisiana, Mississippi, Alabama, and Florida border the Gulf on the north, which are often referred to as the "Third Coast", in comparison with the U.S. Atlantic and Pacific coasts.
Texas is the second largest state in the United States by both area and population. Geographically located in the South Central region of the country, Texas shares borders with the U.S. states of Louisiana to the east, Arkansas to the northeast, Oklahoma to the north, New Mexico to the west, and the Mexican states of Chihuahua, Coahuila, Nuevo León, and Tamaulipas to the southwest, while the Gulf of Mexico is to the southeast.
The economy of the Gulf Coast area is dominated by industries related to energy, petrochemicals, fishing, aerospace, agriculture, and tourism. The large cities of the region are (from west to east) McAllen, Brownsville, Corpus Christi, Houston, Galveston, Beaumont, Lafayette, Baton Rouge, New Orleans, Biloxi, Mobile, Pensacola, St. Petersburg, Tampa, and increasingly, Sarasota. All are the centers of their respective metropolitan areas and contain large ports. (Baton Rouge is relatively far from the Gulf of Mexico; its port is on the Mississippi River, as is the port of New Orleans.)
McAllen is the largest city in Hidalgo County, Texas, United States, and the 22nd-most populous city in Texas. It is located at the southern tip of the state in the Rio Grande Valley. The city limits extend south to the Rio Grande, across from the Mexican city of Reynosa, and McAllen is about 70 mi (110 km) west of the Gulf of Mexico. As of 2017, McAllen’s population was estimated to be 142,696. It is the fifth-most populous metropolitan area in the state of Texas, and the binational Reynosa–McAllen metropolitan area counts a population of nearly 1.52 million.
Brownsville is a city in Cameron County in the U.S. state of Texas. It located on the western Gulf Coast in South Texas, adjacent to the border with Matamoros, Mexico. The city covers 81.528 square miles (211.157 km2) and has a population of 183,299 as of 2017. It is the 131st-largest city in the United States and 16th-largest in Texas. It is part of the Brownsville–Matamoros conurbation, with a population of 1,136,995 people. The city is known for its year-round subtropical climate, deep-water seaport and Hispanic culture.
Corpus Christi, colloquially Corpus, is a coastal city in the South Texas region of the U.S. state of Texas. The county seat of Nueces County, it also extends into Aransas, Kleberg, and San Patricio Counties. It is 130 miles southeast of San Antonio. Its political boundaries encompass Nueces Bay and Corpus Christi Bay. Its zoned boundaries include small land parcels or water inlets of three neighboring counties.
The Gulf Coast is made of many inlets, bays, and lagoons. The coast is also intersected by numerous rivers, the largest of which is the Mississippi River. Much of the land along the Gulf Coast is, or was, marshland. Ringing the Gulf Coast is the Gulf Coastal Plain which reaches from Southern Texas to the western Florida Panhandle while the western portions of the Gulf Coast are made up of many barrier islands and peninsulas, including the 130 miles (210 km) Padre Island and Galveston Island located in the U.S. State of Texas. These landforms protect numerous bays and inlets providing as a barrier to oncoming waves. The central part of the Gulf Coast, from eastern Texas through Louisiana, consists primarily of marshland. The eastern part of the Gulf Coast, predominantly Florida, is dotted with many bays and inlets.
The Mississippi River is the second-longest river and chief river of the second-largest drainage system on the North American continent, second only to the Hudson Bay drainage system. Its source is Lake Itasca in northern Minnesota and it flows generally south for 2,320 miles (3,730 km) to the Mississippi River Delta in the Gulf of Mexico. With its many tributaries, the Mississippi's watershed drains all or parts of 32 U.S. states and two Canadian provinces between the Rocky and Appalachian mountains. The main stem is entirely within the United States; the total drainage basin is 1,151,000 sq mi (2,980,000 km2), of which only about one percent is in Canada. The Mississippi ranks as the fourth-longest and fifteenth-largest river by discharge in the world. The river either borders or passes through the states of Minnesota, Wisconsin, Iowa, Illinois, Missouri, Kentucky, Tennessee, Arkansas, Mississippi, and Louisiana.
A marsh is a wetland that is dominated by herbaceous rather than woody plant species. Marshes can often be found at the edges of lakes and streams, where they form a transition between the aquatic and terrestrial ecosystems. They are often dominated by grasses, rushes or reeds. If woody plants are present they tend to be low-growing shrubs. This form of vegetation is what differentiates marshes from other types of wetland such as swamps, which are dominated by trees, and mires, which are wetlands that have accumulated deposits of acidic peat.
The Gulf Coastal Plain extends around the Gulf of Mexico in the Southern United States and eastern Mexico.
The Gulf Coast climate is humid subtropical, although the southwestern tip of Florida, such as Everglades City, features a tropical climate. Much of the year is warm to hot along the Gulf Coast, while the 3 winter months bring periods of cool (or rarely, cold) weather mixed with mild temperatures. The area is vulnerable to hurricanes as well as floods and severe thunderstorms. Much of the Gulf Coast has a summer precipitation maximum, with July or August commonly the wettest month due to the combination of frequent summer thunderstorms produced by relentless heat and humidity, and tropical weather systems (tropical depressions, tropical storms and hurricanes), while winter and early spring rainfall also can be heavy. This pattern is evident at Houston, Texas, New Orleans, Louisiana, Mobile, Alabama and Pensacola, Florida. However, the central and southern Florida peninsula has a pronounced winter dry season, as at Tampa and Fort Myers, Florida. On the central and southern Texas coast, winter, early spring and mid-summer are markedly drier, and September is the wettest month on average (as at Corpus Christi and Brownsville, Texas). Tornadoes are infrequent at the coast but do occur; however, they occur more frequently in inland portions of Gulf Coast states. Over most of the Gulf Coast from Houston, Texas eastward, extreme rainfall events are a significant threat, commonly from tropical weather systems, which can bring 4 to 10 or more inches of rain in a single day. In August 2017, Hurricane Harvey made landfall along the central Texas coast, then migrated to and stalled over the greater Houston area for several days, producing extreme, unprecedented rainfall totals of over 40 inches (1,000 mm) in many areas, unleashing widespread flooding. Earthquakes are extremely rare to the area, but a surprising 6.0 earthquake in the Gulf of Mexico on September 10, 2006, could be felt from the cities of New Orleans to Tampa.
Everglades City is a city in Collier County, Florida, United States, of which it is the former county seat. As of the 2013 census, the population is 402. It is part of the Naples–Marco Island Metropolitan Statistical Area. The Gulf Coast Visitor Center for Everglades National Park is in Everglades City.
A tropical cyclone is a rapidly rotating storm system characterized by a low-pressure center, a closed low-level atmospheric circulation, strong winds, and a spiral arrangement of thunderstorms that produce heavy rain. Depending on its location and strength, a tropical cyclone is referred to by different names, including hurricane, typhoon, tropical storm, cyclonic storm, tropical depression, and simply cyclone. A hurricane is a tropical cyclone that occurs in the Atlantic Ocean and northeastern Pacific Ocean, and a typhoon occurs in the northwestern Pacific Ocean; in the south Pacific or Indian Ocean, comparable storms are referred to simply as "tropical cyclones" or "severe cyclonic storms".
A flood is an overflow of water that submerges land that is usually dry. In the sense of "flowing water", the word may also be applied to the inflow of the tide. Floods are an area of study of the discipline hydrology and are of significant concern in agriculture, civil engineering and public health.
The Gulf Coast is a major center of economic activity. The marshlands along the Louisiana and Texas coasts provide breeding grounds and nurseries for ocean life that drive the fishing and shrimping industries. The Port of South Louisiana (Metropolitan New Orleans in Laplace) and the Port of Houston are two of the ten busiest ports in the world by cargo volume.As of 2004, seven of the top ten busiest ports in the U.S. are on the Gulf Coast.
The fishing industry includes any industry or activity concerned with taking, culturing, processing, preserving, storing, transporting, marketing or selling fish or fish products. It is defined by the Food and Agriculture Organization as including recreational, subsistence and commercial fishing, and the harvesting, processing, and marketing sectors. The commercial activity is aimed at the delivery of fish and other seafood products for human consumption or as input factors in other industrial processes. Directly or indirectly, the livelihood of over 500 million people in developing countries depends on fisheries and aquaculture.
The term shrimp is used to refer to some decapod crustaceans, although the exact animals covered can vary. Used broadly, shrimp may cover any of the groups with elongated bodies and a primarily swimming mode of locomotion – most commonly Caridea and Dendrobranchiata. In some fields, however, the term is used more narrowly and may be restricted to Caridea, to smaller species of either group or to only the marine species. Under the broader definition, shrimp may be synonymous with prawn, covering stalk-eyed swimming crustaceans with long narrow muscular tails (abdomens), long whiskers (antennae), and slender legs. Any small crustacean which resembles a shrimp tends to be called one. They swim forward by paddling with swimmerets on the underside of their abdomens, although their escape response is typically repeated flicks with the tail driving them backwards very quickly. Crabs and lobsters have strong walking legs, whereas shrimp have thin, fragile legs which they use primarily for perching.
The Port of South Louisiana extends 54 miles (87 km) along the Mississippi River between New Orleans, Louisiana and Baton Rouge, Louisiana, centering approximately at LaPlace, Louisiana, which serves as the Port's headquarters location.
The discovery of oil and gas deposits along the coast and offshore, combined with easy access to shipping, have made the Gulf Coast the heart of the U.S. petrochemical industry. The coast contains nearly 4,000 oil platforms.
Petroleum is a naturally occurring, yellowish-black liquid found in geological formations beneath the Earth's surface. It is commonly refined into various types of fuels. Components of petroleum are separated using a technique called fractional distillation, i.e. separation of a liquid mixture into fractions differing in boiling point by means of distillation, typically using a fractionating column.
Natural gas, also called "Fossil Gas" is a naturally occurring hydrocarbon gas mixture consisting primarily of methane, but commonly including varying amounts of other higher alkanes, and sometimes a small percentage of carbon dioxide, nitrogen, hydrogen sulfide, or helium. It is formed when layers of decomposing plant and animal matter are exposed to intense heat and pressure under the surface of the Earth over millions of years. The energy that the plants originally obtained from the sun is stored in the form of chemical bonds in the gas.
The petrochemical industry is concerned with the production and trade of petrochemicals. It directly interfaces with the petroleum industry, especially the downstream sector. A major part is constituted by the plastics (polymer) industry.
Besides the above, the region features other important industries including aerospace and biomedical research, as well as older industries such as agriculture and — especially since the development of the Gulf Coast beginning in the 1920s and the increase in wealth throughout the United States — tourism.
Before Europeans arrived in the region, the region was home to several pre-Columbian kingdoms that had extensive trade networks with empires such as the Aztecs and the Mississippi Mound Builders. Shark and alligator teeth and shells from the Gulf have been found as far north as Ohio, in the mounds of the Hopewell culture.
The first Europeans to settle the Gulf Coast were primarily the French and the Spanish. The Louisiana Purchase, Adams–Onís Treaty and the Texas Revolution made the Gulf Coast a part of the United States during the first half of the 19th century. As the U.S. population continued to expand its frontiers westward, the Gulf Coast was a natural magnet in the South providing access to shipping lanes and both national and international commerce. The development of sugar and cotton production (enabled by slavery) allowed the South to prosper. By the mid 19th century the city of New Orleans, being situated as a key to commerce on the Mississippi River and in the Gulf, had become the largest U.S. city not on the Atlantic seaboard and the fourth largest in the U.S. overall.
Two major events were turning points in the earlier history of the Gulf Coast region. The first was the American Civil War, which caused severe damage to some economic sectors in the South, including the Gulf Coast. The second event was the Galveston Hurricane of 1900. At the end of the 19th century Galveston was, with New Orleans, one of the most developed cities in the region. The city had the third busiest port in the U.S.and its financial district was known as the "Wall Street of the South". The storm mostly destroyed the city, which has never regained its former glory, and set back development in the region.
Since then the Gulf Coast has been hit with numerous other hurricanes. On August 29, 2005, Hurricane Katrina struck the Gulf Coast as a Category 4 hurricane. It was the most damaging storm in the history of the United States, causing upwards of $80 billion in damages, and leaving over 1,800 dead. Again in 2008 the Gulf Coast was struck by a catastrophic hurricane. Due to its immense size, Hurricane Ike caused devastation from the Louisiana coastline all the way to the Kenedy County, Texas region near Corpus Christi.In addition, Ike caused flooding and significant damage along the Mississippi coastline and the Florida Panhandle Ike killed 112 people and left upwards of 300 people missing, never to be found. Hurricane Ike was the third most damaging storm in the history of the United States, causing more than $25 billion in damage along the coast, leaving hundreds of thousands of people homeless, and sparking the largest search-and-rescue operation in U.S. history.
Other than the hurricanes, the Gulf Coast has redeveloped dramatically over the course of the 20th century. The gulf coast is highly populated. The petrochemical industry, launched with the major discoveries of oil in Texas and spurred on by further discoveries in the Gulf waters, has been a vehicle for development in the central and western Gulf which has spawned development on a variety of fronts in these regions. Texas in particular has benefited tremendously from this industry over the course of the 20th century and economic diversification has made the state a magnet for population and home to more Fortune 500 companies than any other U.S. state. Florida has grown as well, driven to a great extent by its long established tourism industry but also by its position as a gateway to the Caribbean and Latin America. As of 2006, these two states are the second and fourth most populous states in the nation, respectively (see this article). Other areas of the Gulf Coast have benefited less, though economic development fueled by tourism has greatly increased property values along the coast, and is now a severe danger to the valuable but fragile ecosystems of the Gulf Coast.
The following table lists the 15 largest MSAs along the Gulf Coast.
|Rank||Metropolitan Statistical Area||2016 Pop (est.)||2000 Pop||Δ Pop||Combined Statistical Area|
|1||Houston-The Woodlands-Sugar Land, TX MSA||6,772,470||4,715,407||+24.43%||Houston-Baytown-Huntsville, TX CSA|
|2||Tampa-St. Petersburg-Clearwater, FL MSA||3,032,171||2,395,997||+14.66%||primary census statistical area|
|3||New Orleans-Metairie-Kenner, LA MSA||1,268,883||1,316,510||-9.61%||New Orleans-Metairie-Bogalusa, LA CSA|
|4||McAllen-Edinburg-Mission, TX MSA||849,843||569,463||+30.15%||primary census statistical area|
|5||Baton Rouge MSA||835,175||729,361||+11.03%||primary census statistical area|
|6||North Port-Bradenton-Sarasota, FL MSA||788,457||589,959||+16.64%||Sarasota-Bradenton-Punta Gorda, FL CSA|
|7||Cape Coral-Fort Myers, FL MSA||722,336||440,888||+33.12%||primary census statistical area|
|8||Pensacola-Ferry Pass-Brent, FL MSA||485,684||412,153||+10.42%||primary census statistical area|
|9||Corpus Christi, TX MSA||454,726||403,280||+3.18%||Corpus Christi-Kingsville, TX CSA|
|11||Mobile, AL MSA||414,836||399,843||+2.97%||Mobile-Daphne-Fairhope, AL CSA|
|10||Brownsville–Harlingen, TX MSA||422,135||335,227||+18.24%||Brownsville-Harlingen-Raymondville, TX CSA|
|12||Beaumont-Port Arthur, TX MSA||409,968||385,090||-1.72%||primary census statistical area|
|14||Naples-Marco Island, FL MSA||318,537||251,377||+26.72%||primary census statistical area|
|13||Gulfport-Biloxi, MS MSA||365,136||246,190||-3.01%||Gulfport-Biloxi-Pascagoula, MS CSA|
|15||Houma-Bayou Cane-Thibodaux, LA MSA||211,525||194,477||+4.37%||primary census statistical area|
Most of the areas are currently highly populated, and contain many useful and natural resources. Both and close to all are a great place to stay.
|Highway||Significant Cities Served|
|Houston, Baytown, Beaumont, Lake Charles, Lafayette, Baton Rouge, New Orleans, Gulfport, Biloxi, Mobile, Pensacola|
|New Orleans (future), Houma (future), Thibodaux (future), Lafayette|
|Victoria (future), Houston|
|Brownsville, Harlingen, Corpus Christi, Victoria (future)|
|Naples, Fort Myers, North Port, Bradenton, St. Petersburg, Tampa|
|Highway||Significant Cities Served|
|St. Petersburg, Tampa|
|Bradenton, Fort Myers, Naples, St. Petersburg, Tampa|
|Beaumont, Port Arthur|
|Brownsville, Corpus Christi, Harlingen, Victoria|
|Port Lavaca, Victoria|
|Beaumont, Biloxi, Crestview, Houma, Houston, Lafayette, Lake Charles, Mobile, New Orleans, Pascagoula, Pensacola, Thibodaux|
|St. Petersburg, Tampa|
|Beaumont, Port Arthur|
|Fort Walton Beach, Mobile, Pensacola, Panama City|
|Highway||Significant Cities Served|
|Grand Isle, Port Fourchon, Thibodaux|
|Crestview, Fort Walton Beach|
|Houston, Bay City, Port Lavaca, Rockport, Corpus Christi|
|Houston, Lake Jackson, Freeport|
|George Bush Intercontinental Airport - Houston|
|Louis Armstrong New Orleans International Airport|
|Southwest Florida International Airport|
|Tampa International Airport|
|William P. Hobby Airport - Houston|
|Train||Route||Gulf Coast Cities Served|
|City of New Orleans||Chicago to New Orleans||New Orleans|
|Crescent||New York to New Orleans||New Orleans, Picayune, MS, Slidell, LA|
|Sunset Limited||Los Angeles to Orlando (temporarily New Orleans)||Bay St. Louis, MS , Beaumont, TX, Biloxi , Crestview, FL , Gulfport, MS , Houston, Lafayette, LA, Lake Charles, LA, Baton Rouge, LA, Mobile , New Orleans, Panama City, FL , Scriever, LA, Pascagoula, MS , Pensacola|
The Gulf Intracoastal Waterway is the portion of the Intracoastal Waterway located along the Gulf Coast of the United States. It is a navigable inland waterway running approximately 1,050 mi (1,690 km) from Carrabelle, Florida, to Brownsville, Texas.
Southeast Texas is a sub-region of East Texas located in the southeast corner of the U.S. state of Texas. The sub-region is geographically centered on the Houston–Sugar Land–The Woodlands, and Beaumont–Port Arthur metropolitan areas.
Hurricane Juan was a large and erratic tropical cyclone that looped twice near the Louisiana coast, causing widespread flooding. It was the tenth named storm of the 1985 Atlantic hurricane season, forming in the central Gulf of Mexico in late October. Juan moved northward after its formation, and was subtropical in nature with its large size. On October 27, the storm became a hurricane, reaching maximum sustained winds of 85 mph (140 km/h). Due to the influence of an upper-level low, Juan looped just off southern Louisiana before making landfall near Morgan City on October 29. Weakening to tropical storm status over land, Juan turned back to the southeast over open waters, crossing the Mississippi River Delta. After turning to the northeast, the storm made its final landfall just west of Pensacola, Florida, late on October 31. Juan continued quickly to the north and was absorbed by an approaching cold front, although its moisture contributed to a deadly flood event in the Mid-Atlantic states.
Hurricane Audrey was one of the deadliest tropical cyclones in U.S. history, as well as the strongest June hurricane ever recorded in the Atlantic basin, tied with Hurricane Alex in 2010. The rapidly developing storm struck southwestern Louisiana as a powerful Category 3 hurricane, destroying coastal communities with a powerful storm surge that penetrated as far as 20 mi (32 km) inland. The first named storm and hurricane of the annual hurricane season, it formed on June 24 from a tropical wave which moved into the Bay of Campeche. Situated within ideal conditions for tropical development, Audrey quickly strengthened, reaching hurricane status a day afterwards. Moving northwards, it continued to strengthen and accelerate as it approached the United States Gulf Coast. On June 27, the hurricane reached peak sustained winds of 125 mph (205 km/h), making it a major hurricane. At the time, Audrey had a minimum barometric pressure of 946 mbar. The hurricane made landfall at the same intensity between the mouth of the Sabine River and Cameron, Louisiana later that day, causing unprecedented destruction across the region. Once inland, Audrey weakened and turned extratropical over West Virginia on June 29.
The 1915 Galveston hurricane was a deadly hurricane that struck Leeward Islands, Hispaniola, Cuba and Texas, in mid August of the 1915 Atlantic hurricane season. Striking Galveston, Texas, 15 years after the 1900 Galveston Hurricane, its 21-ft (6.4-m) waves were slowed by the new Galveston Seawall but changed the beach structure: on August 17, the entire 300-ft (91.5–m) beach was eroded to become an offshore sandbar, later returning partially, but never the same. The 1915 storm caused a great deal of destruction in its path, leaving 275-400 people dead and $50 million in damage.
Hurricane Fern was the sixth named storm and fourth hurricane of the 1971 Atlantic hurricane season. It formed from a tropical wave which interacted with a large trough of low pressure to form Fern, as well as Hurricane Ginger, Tropical Storm Heidi, and a system later designated as Tropical Depression Sixteen, which moved into South Carolina. Fern crossed southeastern Louisiana as a tropical depression on September 4 before swinging back out over the Gulf of Mexico. Fern reached hurricane status on September 8, reaching a peak intensity of 90 mph (140 km/h) before making landfall near Freeport, Texas, two days later.
The 1987 Gulf Coast tropical storm caused flooding along the Gulf Coast of the United States. The second tropical cyclone and first tropical storm of the 1987 Atlantic hurricane season, it originated from a tropical wave in the Gulf of Mexico, southeast of Texas, on August 9. Initially a tropical depression, the cyclone moved north-northwestward and slightly intensified into a tropical storm later that day. By August 10, it made landfall between Galveston and Beaumont. The system weakened after moving inland and turned towards the east and later southeast. Briefly reemerging over the Gulf on August 15, the depression moved onshore a second time in Florida, before dissipating over eastern Georgia on August 17.
Hurricane Flossy originated from a tropical disturbance in the eastern Pacific Ocean and moved across Central America into the Gulf of Mexico as a tropical depression on September 21, 1956, which became a tropical storm on September 22 and a hurricane on September 23. The hurricane peaked with maximum sustained winds of 90 mph (150 km/h) before it struck the central Gulf coast of the United States as a Category 1 hurricane on September 24, and evolved into an extratropical cyclone on September 25. It was the first hurricane to affect oil refining in the Gulf of Mexico. The tropical cyclone led to flooding in New Orleans, and broke a drought across the eastern United States. The death toll was 15, and total damages reached $24.8 million (1956 USD).
Hurricane Florence was the third of four named tropical cyclones to make landfall on the United States during the 1988 Atlantic hurricane season. The seventh tropical storm and second hurricane of the season, Florence developed on September 7 from an area of convection associated with a dissipating frontal trough in the southern Gulf of Mexico. After initially moving eastward, the storm turned northward and strengthened. Florence reached hurricane status and later peak winds of 80 mph (130 km/h) on September 9 shortly before striking southeastern Louisiana. The storm rapidly weakened over land and dissipated on September 11 over northeastern Texas.
Tropical Storm Felice was a modest tropical cyclone that lightly affected parts of the Gulf Coast of the United States in mid-September 1970. Spawned by an upper-level trough over the Bahamas, the system crossed the Florida Keys and entered the Gulf of Mexico, where it gradually began to strengthen. Felice was a disorganized storm for its entire duration, plagued by dry air, a lack of deep thunderstorm activity, and an ill-defined center of circulation, but nevertheless managed to peak as a high-end tropical storm with winds just below Category 1 hurricane strength. Tracking northwestward, the storm brushed southern Louisiana on September 15 before making landfall northeast of Galveston, Texas, late that same day. Once ashore, Felice quickly deteriorated as it recurved into the central United States. While over southeastern Oklahoma, however, its remnants still closely resembled a formidable tropical cyclone.
The 1812 Louisiana Hurricane was a major hurricane that struck New Orleans, Louisiana, during the War of 1812. It was the worst storm of the early history of New Orleans and was very likely the hurricane which made the closest landfall known to affect the city.
Hurricane Ike was a powerful tropical cyclone that swept through portions of the Greater Antilles and Northern America in September 2008, wreaking havoc on infrastructure and agriculture, particularly in Cuba and Texas. The ninth tropical storm, fifth hurricane, and third major hurricane of the 2008 Atlantic hurricane season, Ike developed from a tropical wave west of Cape Verde on September 1 and strengthened to a peak intensity as a Category 4 hurricane over the open waters of the central Atlantic on September 4 as it tracked westward. Several fluctuations in strength occurred before Ike made landfall on eastern Cuba on September 8. The hurricane weakened prior to continuing into the Gulf of Mexico, but increased its intensity by the time of its final landfall on Galveston, Texas on September 13. The remnants of Ike continued to track across the United States and into Canada, causing considerable damage inland, before dissipating two days later.
The Ike Dike is a proposed coastal barrier that, when completed, would protect the Galveston Bay in Texas, United States. The project would be a dramatic enhancement of the existing Galveston Seawall, complete with floodgates, which would protect more of Galveston, the Bolivar Peninsula, the Galveston Bay Area, and Houston. The barrier would extend across Galveston Island and the Bolivar Peninsula and would provide a barrier against all Gulf surges into the bay. The project is primarily the suggestion of Dr. Bill Merrell of Texas A&M University at Galveston. The Ike Dike would be able to withstand ~10,000 year storms.
The History of Galveston, Texas, begins with the archaeological record of Native Americans who used the island. The first European settlements on the island were constructed around 1816. The Port of Galveston was established in 1825 by the Congress of Mexico following its successful revolution from Spain. The city served as the main port for the Texas Navy during the Texas Revolution. Galveston was founded in 1836 by Matthew Sabo and served as the capital of the Republic of Texas. The Battle of Galveston was fought in Galveston Bay during the American Civil War when Confederate forces under Major General John B. Magruder attacked and expelled occupying Union troops from the city.
The 1941 Texas hurricane, the second storm of the 1941 Atlantic hurricane season, was a large and intense tropical cyclone that struck coastal Texas as a major hurricane in September 1941, causing relatively severe damage. The storm is estimated to have formed in the eastern Gulf of Mexico on September 16. After attaining hurricane strength, it completed a clockwise loop and turned northwestward. The hurricane continued to strengthen until it made landfall near East Matagorda Bay, Texas, with winds of 125 miles per hour (201 km/h), but rapidly weakened as it headed inland. Damage from the storm amounted to about $6.5 million, and crops throughout the region were largely destroyed. The city of Houston suffered extensive damage as the storm passed to the east. The hurricane disrupted activities related to the Louisiana Maneuvers. Later, the system became extratropical and passed over Lake Huron, killing three people in Toronto. Overall, seven people lost their lives due to the cyclone.
United States Coast Guard Air Station Houston is a United States Coast Guard Air Station located 15 miles (24 km) southeast of downtown Houston, Texas on board the Ellington Field Joint Reserve Base (JRB).
Hurricane Debra was a destructive tropical cyclone that developed during the 1959 Atlantic hurricane season. The fifth tropical storm and third hurricane of the season, Debra originated from the interaction of a cold-core low and a tropical wave on July 15. The system was designated a tropical depression on July 23 when it was south of Louisiana and meandered westward while it swiftly intensified into a tropical storm along the Gulf Coast of the United States. A turn towards the northwest became evident as it attained Category 1 hurricane status on the Saffir–Simpson Hurricane Scale the following day while it organized into a developed storm. As the hurricane curved northward at a slow forward speed, strength was maintained as it approached the coast of Texas as a minimal hurricane. It came ashore during the evening of July 24 local time between Freeport and Galveston, Texas. It rapidly weakened into a tropical storm and later a depression as it moved inland, and dissipated on July 28 while it turned northwestward. The remnant moisture later sparked upper-level thunderstorms in late July and early August.
The 1920 Louisiana hurricane was a strong tropical cyclone that caused significant damage in parts of Louisiana in September 1920. The second tropical storm and hurricane of the annual hurricane season, it formed from an area of disturbed weather on September 16, 1920, northwest of Colombia. The system remained a weak tropical depression as it made landfall on Nicaragua, but later intensified to tropical storm strength as it moved across the Gulf of Honduras, prior to making a second landfall on the Yucatán Peninsula. Once in the Gulf of Mexico, the storm quickly intensified as it moved towards the north-northwest, reaching its peak intensity as a Category 2 hurricane with winds of 100 mph (160 km/h) prior to making landfall near Houma, Louisiana with no change in intensity. Afterwards, it quickly weakened over land, before dissipating on September 23 over eastern Kansas.
Racer's hurricane was a destructive tropical cyclone that had severe effects on northeastern Mexico and the Gulf Coast of the United States in early October 1837. It takes its name from the Royal Navy ship Racer, which sustained some damage when it encountered the hurricane in the northwestern Caribbean Sea. The storm first affected Jamaica with flooding rainfall and strong winds on September 26 and 27, before entering the Gulf of Mexico by October 1. As the hurricane approached northern Tamaulipas and southern Texas, it slowed to a crawl and turned sharply eastward. The storm battered the Gulf Coast from Texas to the Florida Panhandle between October 3 and 7, and after crossing the Southeastern United States, it emerged into the Atlantic shipping lanes off the Carolinas. For most of the storm's duration, the strongest winds and heaviest rains were confined to the northern side of its track.