Meteorological history | |
---|---|
Formed | 1 October 2005 |
Dissipated | 5 October 2005 |
Category 1 hurricane | |
1-minute sustained (SSHWS/NWS) | |
Highest winds | 80 mph (130 km/h) |
Lowest pressure | 977 mbar (hPa);28.85 inHg |
Overall effects | |
Fatalities | 1,673 [nb 1] |
Damage | $3.96 billion (2005 USD) |
Areas affected | Costa Rica,Nicaragua,Honduras,El Salvador,Belize,Guatemala,Yucatan Peninsula and Southern Mexico |
IBTrACS | |
Part of the 2005 Atlantic hurricane season |
Hurricane Stan was the deadliest tropical cyclone of the 2005 Atlantic hurricane season. A relatively weak system that affected areas of Central America and Mexico in early October 2005,Stan was the eighteenth named storm and eleventh hurricane of the 2005 season,having formed from a tropical wave on October 1 after it had moved into the western Caribbean. The depression slowly intensified,and reached tropical storm intensity the following day,before subsequently making its first landfall on the Yucatán Peninsula. While traversing the peninsula,the tropical storm weakened,but was able to re-intensify once it entered the Bay of Campeche. Under favorable conditions for tropical cyclogenesis,Stan attained hurricane strength on October 4,and later reached peak intensity with winds of 80 mph (130 km/h) and a minimum barometric pressure of 977 mbar (28.9 inHg). The hurricane maintained this intensity until landfall in the Mexican state of Veracruz later the same day. Once over the mountainous terrain of Mexico,however,Stan quickly weakened,and dissipated on October 5.
Due to Stan's position within a large area of convective activity and thunderstorms,the hurricane's effects were far-reaching and widespread across Central America. Flash floods generated by the hurricane caused severe crop losses,particularly to coffee crops. Overall,Stan caused at least 1,673 deaths across six countries,with many others unaccounted for. Most of these fatalities occurred in Guatemala,and were mostly caused by mudslides triggered by torrential rainfall. The floods in Guatemala destroyed entire towns and disrupted exportation of petroleum. In Mexico,the heavy rains triggered additional mudslides and caused rivers to overflow,flooding nearby villages. Despite being relatively far from Stan as opposed to other countries,El Salvador was also severely affected by the hurricane. The Santa Ana Volcano erupted while Stan was producing heavy rains in the country,which contributed to the damage already wrought by mudslides. Transportation in the country was disrupted. Across the region,Stan caused $3.9 billion in damages,primarily due to torrential rainfall.
A tropical wave left the west coast of Africa on 17 September 2005, which the National Hurricane Center considered the likely origin of Hurricane Stan. For several days, the wave moved westward across the tropical Atlantic Ocean without any signs of development. The associated thunderstorms, or convection, increased on September 22, although the presence of wind shear prevented further organization. The wave entered the eastern Caribbean Sea on September 25. [1] Around that time, the NHC identified the wave in their tropical weather outlook, noting that "any development [would] be slow to occur." [2] The thunderstorms became more consolidated by September 27, as upper-level conditions became more favorable. [1] [3] The system's organization fluctuated, developing a weak circulation and broad low-pressure area on September 28 over the western Caribbean Sea. [3] [4] The Hurricane Hunters flew into the system on September 29, observing a broad area of thunderstorms with insufficient organization to be classified a tropical cyclone. [5] Over several days, the system failed to consolidate and was "slowly festering", as described by NHC forecaster Stacy Stewart. On October 1, the circulation became more defined, developing into Tropical Depression Twenty about 215 km (130 mi) southeast of Cozumel. [1] [6]
Upon its development, the depression's circulation was broad, with several small vorticities. The associated convection developed outflow as the overall system moved generally westward, steered by a ridge over the northern coast of the Gulf of Mexico. The NHC anticipated that the system's passage over the Yucatán Peninsula would tighten the wind field and allow for further development in the Bay of Campeche. [6] [7] Early on October 2, the depression intensified into Tropical Storm Stan, and at 10:00 UTC that day it made landfall in eastern Mexico near Punta Hualaxtoc, Mexico, roughly 35 mi (55 km) south of Tulum. [1] For much of its duration, Stan was associated with a Central American gyre, which was a much larger circulation covering eastern Mexico and Central America. [1] [8] After moving ashore the Yucatán, Stan traversed the peninsula in about 18 hours, emerging into the Bay of Campeche as a tropical depression on October 3. [1]
After emerging into the Bay of Campeche, Stan had a well-defined circulation with an anticyclone aloft, and was moving over an area of nearly 30 °C (86 °F) waters. Thunderstorms soon redeveloped, and the depression quickly reattained tropical storm status. [9] [10] [1] A strong area of high pressure over the western Gulf of Mexico forced the storm to turn southwestward, back to the Mexican coastline. [1] Initially, the convection was mostly limited to the eastern periphery. [11] Early on October 4, the convection increased significantly over the center as well-defined rainbands organized into an eyewall. [1] [12] At 06:00 UTC that day, Stan intensified into a hurricane, and around that time it turned more to the southwest. Six hours later, the hurricane made landfall in the Mexican state of Veracruz near Punta Roca Partida, about 150 km (90 mi) east-southeast of the city of Veracruz. [1] It was the first hurricane landfall in the state since Hurricane Gert in 1993. [13] Stan moved ashore with sustained winds of 80 mph (130 km/h), and a minimum pressure of 28.85 inHg. The storm rapidly weakened over the mountainous terrain, and Stan dissipated early on October 5 over the state of Oaxaca. [1]
After Stan's development, the Government of Mexico issued tropical storm warnings from Chetumal to Cabo Catoche along the eastern Yucatán peninsula, with a tropical storm watch issued westward to the city of Campeche. These were dropped after Stan moved over the Yucatán peninsula. After the storm moved over the Bay of Campeche, Mexico issued hurricane warnings between Cabo Rojo to Punta El Lagarto on October 3, about 27 hours before landfall. Additional warnings were expanded to include more of the coast. [1] The NHC had anticipated that landfall would not occur for 48 hours; it later wrote that the agency had "not predicted very well", describing the southwest path as "unexpected". [1] [14]
Ahead of the storm, state oil company Pemex evacuated 270 employees from five platforms in the Gulf of Mexico, while also closing three oil exporting ports. [15]
In Veracruz state where Stan moved ashore, about 38,000 people evacuated their homes, utilizing thousands of shelters. Schools were canceled in the state. Elsewhere, about 600 families evacuated in Chiapas in areas near the Guatemalan border. [16]
Some 100,000 inhabitants of the Sierra de los Tuxtlas region on the Gulf Coast were evacuated from their homes, and incidents of mild flooding as well as wind damage (such as uprooted trees and roofs ripped off houses) were reported from coastal areas of Veracruz, including the port of Veracruz, Boca del Río, San Andrés Tuxtla, Santiago Tuxtla, Minatitlán and Coatzacoalcos, as well as state capital Xalapa further inland. The armed forces evacuated the inhabitants of a dozen or so towns on the coastal plain, between World Heritage Site Tlacotalpan in the west and the lakeside resort of Catemaco in the east.
Country | Fatalities | Damage (USD) | Refs |
---|---|---|---|
Costa Rica | 1 | 20 million | [17] |
El Salvador | 69 | 356 million | [17] [18] |
Guatemala | 1,513 | 996 million | [19] [20] |
Honduras | 7 | 100 million | [21] |
Mexico | 80 | 2.5 billion | [1] [17] |
Nicaragua | 3 | N/A | [17] |
Total | 1,673 | 3.96 billion |
Throughout its duration, Hurricane Stan was embedded within a larger Central American gyre, which resulted in a large area of thunderstorms across Mexico and Central America. This led to torrential rainfall and flooding that killed thousands of people, mostly in Guatemala. [1]
Hundreds were reported missing and were feared dead throughout the region. One estimate put the death toll above 2,000 in Guatemala alone. The final death toll will likely never be known due to the extensive decomposition of bodies in the mud. [22]
Greenpeace blamed rampant deforestation for exacerbating the disaster, and called on governments to do more to protect local woods and mangroves. [23]
Across southeastern Mexico, Hurricane Stan dropped heavy rainfall, resulting in damaging floods that killed 98 people. [13] The hurricane produced a peak 24 hour rainfall total of 307 mm (12.1 in) in Novillero, Chiapas. When it struck the Yucatán, Stan became the record sixth storm of the year to hit Mexico. As it moved across the peninsula, it dropped 137.5 mm (5.41 in) of precipitation in Cancún. The storm produced floods and landslides across eight states in southeastern Mexico, with the most severe effects in Chiapas, Veracruz, Oaxaca, Puebla and Quintana Roo. [24] The hurricane's damage across the five states was estimated at Mex$13.7 billion (US$1.28 billion), with the most damage and fatalities occurring in Chiapas, where 86 people died. In addition to the direct damage, Stan resulted in another Mex$7.29 billion (US$670 million) worth of indirect damages, such as loss of productivity to businesses. Across the region, the hurricane damaged 55,038 houses, as well as 1,553 schools, and had damaging effects to an estimated 326,621.1 hours (1,175,836 ks ) worth of crops or grasslands. Stan's passage also disrupted the transportation network, damaging 17,569.5 km (10,917.2 mi) worth of roadways. [13]
The most damage and fatalities occurred in Chiapas, where the rainfall amounts were six times the October average. In mountainous portions of the state, the intense rainfall caused 98 rivers to overflow. Floods and mudslides affected much of Chiapas, with monetary damage costs estimated at Mex$8.8 billion (US$819 million), representing about 5% of the state's Gross Domestic Product (GDP). An additional Mex$6.2 billion (US$582 million) in economic losses resulted from loss of productivity caused by the hurricane's effects. The hurricane damaged or destroyed 32,514 houses, and flooded thousands more, which displaced about 92,000 people from their homes, with the most damage in Tapachula, Huixtla, Siltepec, and Motozintla. About 68% of the damaged houses occurred in small towns in rural areas. Officials opened 41 emergency shelters across the state, which housed 83,825 people. The storm also damaged 2,307 businesses, mostly impacting machinery and the supplies of small companies. Disrupted or blocked roads temporarily isolated about 700,000 people, which impacted search-and-rescue efforts, with 38 bridges damaged. The hurricane also damaged 114 health centers, including six rural clinics that were destroyed. Of the 305 schools damaged across the state, 111 were destroyed, with 12% of the students across Chiapas affected by the storm. Water and sewage systems were also damaged, affecting 353,000 people. The storm knocked down 2,300 power poles and another 585 transmission towers across the state, affecting more than 81,000 people. The floods inundated the boardwalk at Chiapa de Corzo with 1 m (3.3 ft) of mud. Across the state, the storm heavily damaged the corn, coffee, and banana crops, while also killing thousands of livestock and beehives. [13]
Outside of Chiapas, the hurricane damage was heaviest in the state of Veracruz, with economic costs estimated at Mex$2.535 billion (US$236 million). Rainfall in the state reached 566 mm (22.3 in) at a station called El Tejar, located near where Stan moved ashore. [13]
As a tropical storm, Stan brought torrential rainfall and gusty winds to parts of the Yucatán Peninsula. Flash flooding took place in several areas; however, no loss of life was reported. [25]
As the system progressed inland towards the Sierra Madre del Sur to the west of the Isthmus of Tehuantepec, the states of Oaxaca and Chiapas were affected with torrential rains.
Some areas in the Sierra Norte, in the central state of Puebla, were also flooded. Three people died in a mudslide at Xochiapulco Hill.
The Ministry of the Interior declared states of emergency in the worst hit municipalities of five states: Chiapas, Hidalgo, Oaxaca, Puebla, and Veracruz. According to Mexican president Vicente Fox, Hurricane Stan wrought roughly 20 billion pesos (US$1.9 billion) in damage throughout the country. [26]
By 11 October 2005, at least 1,500 people were confirmed to have died, and up to 3,000 were believed missing. Many communities were overwhelmed, and the worst single incident appears to have occurred in Panabaj, an impoverished Maya village in the highlands near Lake Atitlán in Sololá department. This volcanic lake was so overwhelmed by the torrential rains that many of the small, Mayan villages covering the shores experienced landslides from above. Some of the towns were so overwhelmed by the slides that the mayor has declared them graveyards, and all people who are missing are counted as dead. Piedra Grande, a hamlet in the municipality of San Pedro Sacatepéquez, was also destroyed. Floods and mudslides obliterated the community of about 1,400 people, and it was feared that most or all of the population of the community lost their lives. The government stated that it did not know what was going on in the southwest of the country, and particularly in the San Marcos department because a vital bridge was destroyed at El Palmar, Quetzaltenango, cutting the region off from the rest of the country. There were reported petrol shortages, including in Quetzaltenango.[ citation needed ]
A large portion of the figure comes from one village alone, as a mudslide completely destroyed the village of Panabaj in Guatemala's Sololá department.
The October 1 eruption of the Santa Ana Volcano, located near the capital San Salvador, compounded the problems, which led to even more destructive floods and mudslides from Stan.
Damage from Stan and the volcano was estimated at $355.6 million (2005 USD), equivalent to 2.2% of the country's GDP from the previous year. [18]
A state of emergency was declared. According to the director of El Salvador's National Emergency Centre, 300 communities were affected by the floods, with over 54,000 people forced to flee their homes. A state of emergency also was called for in Guatemala by President Óscar Berger where 36,559 people were reported in emergency shelters. Some looting was also reported, a scene reminiscent of Hurricane Katrina five weeks previous.[ citation needed ]
A spokesman for the Salvadoran Red Cross said that "the emergency is bigger than the rescue capacity, we have floods everywhere, bridges about to collapse, landslides and dozens of roads blocked by mudslides". The Pan-American Highway was cut off by mudslides leading into the capital, San Salvador, as well as several other roads. 72 deaths were confirmed in El Salvador.
Eight of the deaths in Nicaragua were as a result of a boat carrying migrants from Ecuador and Peru that ran ashore.
Throughout Honduras, heavy rains produced by Hurricane Stan resulted in seven fatalities and roughly $100 million in losses. [21]
Because of the severe damage and extensive loss of life wrought by the storm, the name Stan was retired from the Atlantic hurricane naming lists in April 2006 by the World Meteorological Organization. The name will never again be used for another tropical cyclone in the Atlantic basin. It was replaced with Sean for the 2011 Atlantic hurricane season. [27] [28]
The widespread damage across Mexico resulted in a state of emergency across five states, including 41 municipalities in Chiapas. There, relief supplies utilized Port Chiapas to distribute more than 2,000 tons of relief supplies. Helicopters airlifted supplies to 16,434 people across Chiapas, and occurred with such frequency that in Tapachula, helicopters left every five minutes in the weeks following the storm. Thousands of workers cleared and repaired roads. Mexico's Secretariat of Social Development hired 1,804 cooks and set up 270 temporary kitchens to feed people in the aftermath of the storm. Also in the state, officials encouraged a "Host Family" program, in which friends, family, or neighbors would temporarily house people left homeless by Stan, and in exchange receive food and cleaning supplies; about 1,200 families ultimately participated in the program. Hundreds of medical teams provided about 220,000 consultations to affected people across Chiapas. This included a program that helped more than 6,000 people deal with the psychological stresses of the storm. Health workers also cleaned water wells and fumigated areas to prevent the spread of dengue fever. Following the damaging effects in the state of Hidalgo, officials sent medical teams to 1,556 houses to stop the spread of diseases. In January and February 2006, workers from Mexico's Centro Nacional de Prevención de Desastres, or CENAPRED, visited the five most affected states to assess and assess the effects from the storm. [13]
Hurricane Keith was an Atlantic hurricane in October 2000 that caused extensive damage in Central America, especially in Mexico and Belize. It was the fifteenth tropical cyclone, eleventh named storm, and seventh hurricane of the 2000 Atlantic hurricane season. Keith developed as a tropical depression from a tropical wave in the western Caribbean Sea on September 28. The depression gradually strengthened, and became Tropical Storm Keith on the following day. As the storm tracked westward, it continued to intensify and was upgraded to a hurricane on September 30. Shortly thereafter, Keith began to rapidly deepen, and peaked as a Category 4 hurricane less than 24 hours later. Keith then began to meander erratically offshore of Belize, which significantly weakened the storm due to land interaction. By late on October 2, Keith made landfall in Ambergris Caye and Caye Caulker, Belize as a minimal hurricane. It quickly weakened to a tropical storm, before another landfall occurred near Belize City early on the following day. While moving inland over the Yucatán Peninsula, Keith weakened further, and was downgraded to a tropical depression before emerging into the Gulf of Mexico on October 4. Once in the Gulf of Mexico, Keith began to re-strengthen and was upgraded to a tropical storm later that day, and a hurricane on the following day. By late on October 5, Keith made its third and final landfall near Tampico, Tamaulipas, Mexico as a moderately strong Category 1 hurricane. The storm quickly weakened inland and dissipated as a tropical cyclone by 24 hours after landfall.
Hurricane Roxanne was a rare and erratic tropical cyclone that caused extensive flooding in Mexico due to its unusual movement. The seventeenth storm, tenth hurricane, and the fifth and final major hurricane of the very active 1995 Atlantic hurricane season, Roxanne developed in the southwestern Caribbean Sea from an area of low pressure on October 7. The depression curved northward, causing it to avoid landfall in Central America. By October 9, the depression intensified enough to be upgraded to Tropical Storm Roxanne. On the following day, Roxanne turned west-northward, where it promptly intensified into a hurricane. As Roxanne headed generally westward, it began to rapidly deepen and reached Category 3 intensity less than 24 hours after becoming a hurricane. Shortly thereafter, Roxanne made landfall near Cozumel, Mexico at its peak intensity, which caused severe damage.
Hurricane Diana was a deadly tropical cyclone which made landfall in Mexico in August 1990. The fourth named storm and second hurricane of the season, Diana developed from a tropical wave in the southwestern Caribbean on August 4. Forming as a tropical depression, the system brushed Honduras before intensifying into a tropical storm the following day. Continuing to gradually strengthen, Diana made its first landfall in Mexico's Yucatán Peninsula as a strong tropical storm late on August 5. The cyclone weakened slightly due to land interaction, before emerging into the Bay of Campeche on August 6. Once over water, warm sea surface temperatures allowed Diana to quickly become a hurricane and later peak as a Category 2 on the Saffir–Simpson hurricane scale on August 7. Shortly thereafter, the storm made landfall near Tampico, Tamaulipas, with winds of 100 mph (160 km/h). Rapid weakening ensued once the storm moved over the high terrain of Mexico, with Diana diminishing to a tropical depression roughly 24 hours after moving onshore. The cyclone later emerged into the Gulf of California on August 9 shortly before dissipating. The remnant disturbance was monitored until losing its identity over Arizona on August 14.
Tropical Storm Jose was a short-lived tropical storm which made landfall in central Mexico during August 2005. Jose was the tenth named storm of the 2005 Atlantic hurricane season and the fourth of six tropical cyclones to make landfall in Mexico in that year.
Tropical Storm Arlene brought torrential rainfall to the western United States Gulf Coast, particularly to the U.S. state of Texas, in June 1993. The first named storm of the 1993 Atlantic hurricane season, Arlene developed from an area of low pressure in the Bay of Campeche on June 18. The depression slowly strengthened as it tracked west-northwestward and later north-northwestward across the western Gulf of Mexico. Arlene was subsequently upgraded to a tropical storm on June 19, but failed to intensify further due to its proximity to land. The cyclone then made landfall on Padre Island, Texas, with winds of 40 mph (65 km/h) and degenerated into a remnant disturbance on June 21.
Tropical Storm Larry was the twelfth named tropical storm in the 2003 Atlantic hurricane season. It was one of eight storms to impact Mexico from either the Pacific or Atlantic oceans in the season. Larry formed in early October from an extratropical storm in the Bay of Campeche, and reached a peak intensity of 65 mph (105 km/h). Due to weak steering currents, the storm moved southward, which resulted in the storm making landfall on the Tabasco coastline. It was the first tropical storm to strike the region since Tropical Storm Brenda in 1973.
Hurricane Barbara was the easternmost landfalling Pacific hurricane on record. As the first hurricane of the 2013 Pacific hurricane season, Barbara developed from a low-pressure area while located southeast of Mexico on May 28. It headed slowly north-northeastward and strengthened into a tropical storm early on the following day. After recurving to the northeast, Barbara intensified into a Category 1 hurricane on May 29 and made landfall in Chiapas at peak intensity with winds of 80 mph (130 km/h) and a barometric pressure estimated at 983 mbar. When the hurricane made landfall, it was the second earliest landfalling hurricane in the basin since reliable records began in 1966. Barbara then moved across the Isthmus of Tehuantepec and dissipated within the mountainous terrain of Sierra Madre de Chiapas on May 30.
Tropical Storm Olaf was an erratic and long-lived tropical cyclone that brought heavy rainfall to regions of Mexico, which would be devastated by Hurricane Pauline a week later. The sixteenth named storm of the 1997 season, Olaf formed on September 26 off the southern coast of Mexico. It moved northward and quickly intensified, reaching peak winds of 70 mph (110 km/h) before weakening and hitting Oaxaca as a tropical depression. In Mexico, El Salvador, and Guatemala, the system brought heavy rainfall, which killed 18 people and caused flooding and damage. It was originally thought that Olaf dissipated over Mexico, although its remnants continued westward for a week. It interacted with Hurricane Pauline, which caused Olaf to turn to the southeast and later to the north to strike Mexico again, finally dissipating on October 12.
Tropical Storm Hermine caused significant flooding in Mexico during September 1980. The eleventh tropical cyclone and eight named storm of the 1980 Atlantic hurricane season, Hermine developed from a tropical wave that emerged into the Atlantic from the west coast of Africa on September 11. After uneventfully crossing the Atlantic Ocean, the system developed a well-defined circulation while in the Caribbean Sea on September 20 and was then classified as a tropical depression. After becoming a tropical cyclone, the depression steadily strengthened as it tracked nearly due westward. By September 21, it strengthened into Tropical Storm Hermine and brushed the northern coast of Honduras shortly thereafter. It nearly became a hurricane before it made landfall in Belize on September 22. After weakening over the Yucatan Peninsula, Hermine restrengthened to near-hurricane status again over the Gulf of Mexico before making landfall in the Mexican state of Veracruz. Hermine steadily weakened inland and eventually dissipated on September 26.
Tropical Storm Matthew was a weak but deadly and destructive tropical cyclone which made landfall in Central America during the 2010 Atlantic hurricane season. The fifteenth tropical cyclone and thirteenth named storm of the year, Matthew formed on September 23 and lost its tropical characteristics in the morning of September 26. However, its remnants continued to produce life-threatening rain over parts of Central America as it dissipated.
Tropical Storm Arlene, the first named storm of the 2011 Atlantic hurricane season, brought blustery conditions to much of eastern Mexico in late June to early July 2011. Arlene originated from an Atlantic tropical wave, which crossed the Yucatán Peninsula before emerging over warm waters in the Bay of Campeche. Despite moderate wind shear, the disturbance strengthened and developed a surface circulation, prompting the National Hurricane Center to declare it a tropical storm on June 28. Arlene remained vigorous for most of its existence; the storm peaked in intensity with winds of 65 mph (100 km/h) on June 30, just before making landfall on the coast of Veracruz. Crossing the mountains of eastern Mexico, Arlene weakened to a depression before dissipating early on July 1.
Tropical Storm Fernand was a short-lived but deadly tropical cyclone that struck parts of Veracruz state, Mexico, causing flash flooding and landslides. The sixth tropical storm of the 2013 Atlantic hurricane season, Fernand developed from the merger of two tropical waves that had moved off the coast of Africa in the Bay of Campeche on August 25. Quickly organizing, the cyclone strengthened into a tropical storm and eventually made landfall on the coast of Mexico as a moderate to strong tropical storm. Fernand persisted for another day inland before dissipating over the mountainous terrain of the country. During its relatively short lifespan, Fernand caused numerous flash floods in its wake which resulted in the deaths of 14 people in and around the areas of Veracruz.
Hurricane Ingrid was one of two tropical cyclones, along with Hurricane Manuel, to strike Mexico within a 24-hour period, the first such occurrence since 1958. Ingrid was the ninth named storm and second hurricane of the 2013 Atlantic hurricane season. It formed on September 12 in the Gulf of Mexico from a broad disturbance that also spawned Manuel in the eastern Pacific. After initially moving westward toward Veracruz, Ingrid turned northeastward away from the coast. Favorable conditions allowed it to attain hurricane status on September 14, and the next day Ingrid attained peak winds of 140 km/h (85 mph). Subsequently, increased wind shear weakened the convection as the storm turned more to the northwest and west. On September 16, Ingrid made landfall just south of La Pesca, Tamaulipas in northeastern Mexico as a strong tropical storm, and dissipated the next day. The hurricane was also the last one to form in the Gulf of Mexico until Hurricane Hermine in 2016.
Tropical Storm Boris was a weak and short-lived tropical cyclone that brought rainfall to the Isthmus of Tehuantepec and surrounding areas in June 2014. The second named storm of the season, Boris developed from the interaction of a low-level trough and a Kelvin wave south of Mexico late on June 2. Initially a tropical depression, the system moved generally northward and strengthened into Tropical Storm Boris by midday on June 3. About six hours later, Boris peaked with maximum sustained winds of 45 mph (75 km/h) – indicative of a weak tropical storm. By early on June 4, interaction with land caused the storm to weaken, deteriorating to a tropical depression. Later that day, Boris degenerated into a remnant low pressure, before fully dissipating over the Gulf of Tehuantepec on June 5.
Tropical Storm Harvey was the final tropical cyclone in a record-breaking string of eight consecutive storms that failed to attain hurricane intensity. The eighth tropical cyclone and eighth named storm of the 2011 Atlantic hurricane season, Harvey developed from a tropical wave in the western Caribbean Sea on August 19. It moved over warm waters in the vicinity of Central America. Later on August 19, the system strengthened into Tropical Storm Harvey while just offshore Honduras. Additional organization occurred and Harvey attained its peak intensity of 65 mph (100 km/h) prior to coming ashore Belize on August 20. Harvey weakened to a tropical depression on August 21, but re-intensified to a tropical storm after emerging into the Bay of Campeche. Early on August 22, it made landfall in Veracruz, then weakened and dissipated several hours later.
Hurricane Katia was a strong Atlantic hurricane which became the most intense storm to hit the Bay of Campeche since Karl in 2010. The eleventh named storm and sixth hurricane of the exceptionally active 2017 Atlantic hurricane season, Katia originated on September 5, out of a broad low-pressure area that formed in the Bay of Campeche. Located in an area of weak steering currents, Katia meandered around in the region, eventually intensifying into a hurricane on September 6. The nascent storm eventually peaked as a 105 mph (165 km/h) Category 2 hurricane on the Saffir–Simpson scale while it began to move southwestward. However, land interaction began to weaken the hurricane as it approached the Gulf Coast of Mexico. Early on September 9, Katia made landfall near Tecolutla at minimal hurricane intensity. The storm quickly dissipated several hours later, although its mid-level circulation remained intact and later spawned what would become Hurricane Otis in the Eastern Pacific.
Tropical Storm Amanda and Tropical Storm Cristobal were two related, consecutive tropical storms that affected Central America, southern Mexico, the Central United States, and Canada in late May and early June 2020. The first tropical cyclone formed in the East Pacific and was named Amanda. After crossing Central America, it regenerated into a second one in the Gulf of Mexico and was named Cristobal. Amanda was the second tropical depression and the first named storm of the 2020 Pacific hurricane season, and Cristobal was the third named storm of the extremely active 2020 Atlantic hurricane season, and the earliest third named storm in the North Atlantic Ocean on record. Cristobal's regeneration date in the North Atlantic eclipsed the date set by Tropical Storm Colin in 2016, which formed on June 5. It was also the first Atlantic tropical storm formed in the month of June since Cindy in 2017, and the first June tropical cyclone to make landfall in Mexico since Danielle in 2016.
Hurricane Nana was a small, short-lived tropical cyclone that caused relatively minor damage in Belize and Mexico in early September 2020. The sixteenth tropical cyclone, fourteenth named storm, and fifth hurricane of the record-breaking 2020 Atlantic hurricane season, Nana originated from a tropical wave that moved off the coast of West Africa on August 23. The system progressed westward with little development for the next week before crossing into the Caribbean Sea. The wave gradually developed organized convection and a defined surface low on September 1, signifying the formation of Tropical Storm Nana as it approached Jamaica. Persistent wind shear stifled development of the storm, though following repeated bursts of deep convection, it intensified into a minimal hurricane on September 3. Nana attained peak winds of 75 mph (121 km/h) and a minimum pressure of 994 mbar shortly before striking Belize. Once onshore, the hurricane rapidly degraded and its surface low dissipated over Guatemala on September 4. The mid-level remnants of Nana later reorganized over the Gulf of Tehuantepec and became Tropical Storm Julio.
Hurricane Grace was the strongest tropical cyclone to make landfall in the Mexican state of Veracruz. Grace impacted much of the Leeward Islands and Greater Antilles as a tropical storm, before causing more substantial impacts in the Yucatán Peninsula and Veracruz as a hurricane. It was the seventh named storm, second hurricane, and first major hurricane of the 2021 Atlantic hurricane season. Originating from a tropical wave in the Main Development Region, the primitive system tracked west-northwest across the Atlantic Ocean towards the Antilles, becoming a tropical depression on August 14. It strengthened into Tropical Storm Grace later the same day, but weakened back to a depression due to an unfavorable environment. After moving near Haiti as a tropical depression, it strengthened back to a tropical storm and became a hurricane on August 18, reaching an initial peak intensity with maximum sustained winds of 80 mph (130 km/h) and a pressure of 986 mbar (29.12 inHg). It weakened back to a tropical storm after its landfall in the Yucatán Peninsula and emerged into the Bay of Campeche, entering a very favorable environment for intensification hours later. Grace then rapidly intensified into a Category 3 hurricane with winds of 120 mph (190 km/h) in about 24 hours. The storm made its final landfall in the state of Veracruz at peak intensity and quickly degenerated into a remnant low over mainland Mexico on August 21; however, its remnants later regenerated into Tropical Storm Marty in the Eastern Pacific on August 23.
Tropical Storm Chris was a weak and short-lived tropical cyclone that brought heavy rainfall and flooding to parts of Mexico in early July 2024. The third named storm of the 2024 Atlantic hurricane season, Chris developed from a tropical wave that was first noted by the National Hurricane Center (NHC) on June 24. The wave struggled to organize as it moved westward across the Caribbean Sea and crossed the Yucatán Peninsula on June 30. Upon entering the Bay of Campeche, the wave coalesced into a tropical depression on June 30. Located within a favorable environment for strengthening, the depression intensified into Tropical Storm Chris about six hours later. Shortly thereafter, Chris moved ashore near Alto Lucero, Veracruz. Chris rapidly weakened over the mountainous terrain of East Mexico and dissipated on July 1.