Category 5 hurricane | |
---|---|
1-minute sustained (SSHWS/NWS) | |
Highest winds | 175 mph (280 km/h) |
Lowest pressure | 905 mbar (hPa);26.72 inHg |
Overall effects | |
Fatalities | 13 |
Damage | $184 million (2007 USD) |
Areas affected | Mexico |
Part of the 2007 Atlantic hurricane season | |
History Impact Other wikis |
The effects of Hurricane Dean in Mexico were more severe than anywhere else in the storm's path. Hurricane Dean,the most intense storm of the 2007 Atlantic hurricane season,formed in the Atlantic Ocean west of Cape Verde on August 14,2007. The Cape Verde-type hurricane sped through the Caribbean Sea,rapidly intensifying before making landfall on Mexico's Yucatán Peninsula. Accurate forecasts of the storm's location and intensity enabled thorough preparations;nevertheless when the massive storm made landfall on the Yucatán Peninsula as a catastrophic Category 5 hurricane on the Saffir-Simpson Hurricane Scale it damaged thousands of homes.
Weakening as it crossed the peninsula,Dean emerged into the Bay of Campeche and re-strengthened before making a second landfall in Veracruz. Although the second landfall did not bring winds as intense as the first,it brought more rainfall and caused devastating landslides in the states of Veracruz and Tabasco. Between the two landfalls,Dean caused MXN$2 billion (US$184 million;2007 dollars) of damage and killed 13 people.
Forecasters and computer models at the Miami-based National Hurricane Center predicted that Hurricane Dean would impact the Yucatán Peninsula a full 6 days before the storm actually arrived. [1] [2] The hurricane's stable and well predicted path gave all of the countries in the region ample time to prepare for its arrival. [1] On August 17,at the request of the Quintana Roo state government,which was expecting their state to suffer a direct hit,the Civil Protection Office of Mexico's federal Interior Ministry declared a state of emergency for the entire state. This included the towns and cities of Cancún,Playa del Carmen,and Chetumal as well as the islands of Cozumel,Isla Mujeres and Holbox.
On August 18 authorities began evacuating people from parts of Quintana Roo,moving 2,500 people from Holbox Island [3] [4] and a further 80,000 tourists from elsewhere in the state. [5] Air-evacuations of tourists were stopped [6] when Dean's outer rainbands closed almost a dozen [7] Cancún and Cozumel airports on the evening of August 20. The Campeche airport closed shortly thereafter. [8] The state government set up 530 storm shelters in schools and other public buildings,prepared to hold 73,000 people. [9] With 20,000 food packages ready,the state of Yucatán,Quintana Roo's neighbor to the northwest,declared a green alert indicating a low but significant level of danger. [10] [11]
World Vision and other international aid agencies prepared blankets,sheets,personal hygiene items and medicines for quick transport to affected areas. [12] The United States pre-positioned a three-person disaster management team into the Yucatán before the storm's arrival with the intent of helping coordinate disaster management if necessary. [13] The U.S. State Department urged its citizens in Quintana Roo,Yucatán,and Campeche to prepare for the storm and to evacuate if necessary. The department also relocated its non-essential personnel from those states to Mexico City. [11] At 1500 UTC on August 19 a hurricane watch was issued on the Yucatán Peninsula from Chetumal to San Felipe and final preparations were rushed to completion. [14]
On August 20,warnings for Dean's second landfall were issued. The coast from Progreso to Ciudad del Carmen was put under a hurricane warning and the coast from Cancún at the tip of the Yucatán Peninsula west to Progreso. At 0300 UCT,August 21,a tropical storm watch was issued for the coast from Chilitepec to Veracruz,and a hurricane watch was issued from Chilitepec to Tampico,Tamaulipas. As Dean began to cross the Yucatán Peninsula and maintained its structure better than forecasters had expected,these watches and warnings were expanded. At their peak,a hurricane warning covered the area from Campeche,Campeche,to Coatzacoalcos,Veracruz,and a tropical storm warning stretched from Tampico to La Cruz,Tamaulipas. [1]
Residents in Veracruz stocked up on essential supplies,especially food and water,ahead of the storm's second landfall. [15] At the request of the government of Veracruz,federal Secretary of the Interior Francisco Ramírez Acuña declared a state of emergency for 81 municipalities ahead of Hurricane Dean's expected landfall in the state. This gave local authorities access to the resources of the Revolving Fund of the National Natural Disaster Fund to take care of the nutrition,health,and shelter their populations should the storm's damage require it. [16]
Although Dean was still a hurricane and was expected to re-strengthen slightly before making its second landfall,the fact that it had weakened caused some residents to let down their guard. [17] As a result,residents of Veracruz and Campeche were much less prepared for the storm than those on the Yucatán Peninsula. [1]
The hurricane hit land near Majahual on the Quintana Roo coast of the Yucatán Peninsula at 0830 UTC on August 21. Wind gusts of 200 mph (320 km/h) were reported. The state's tourist cities of Cancún and Cozumel were spared the worst of the storm,but it wreaked havoc in the state capital Chetumal,some 40 mi (64 km) south of landfall,causing significant flooding. [18] Communication with the Mayan communities near the landfall location was initially difficult,but the town of Majahual,which had a population of 200,was "almost flattened" by the storm. Storm surge and high winds severely damaged or destroyed hundreds of buildings [19] and had the strength to crumple steel girders. [1] About 15,000 families were left homeless,primarily in small villages around Quintana Roo. [20] At the Costa Maya cruise port,waves tore away portions of the concrete docks and destroyed the boardwalk. The damage made the port unsuitable for cruise ships,effectively freezing the region's tourism industry until they could be repaired. [19] [21] The hurricane's winds damaged 2.3 million ha (5.7 million acres) of jungle,almost all of it in Quintana Roo,Yucatán,and Campeche. [20]
At its first landfall,the bulk of Hurricane Dean's damage was to agriculture. 12,000 producers suffered losses,mostly in the states of Quintana Roo and Yucatán. 30,000 hectares (74,000 acres) of habanero peppers were destroyed,along with 150,000 hectares (370,000 acres) of corn and 60,000 hectares (150,000 acres) of citrus. Extensive damage to fields planted with bananas,avocados,cucumbers,squash,jalapeño peppers,and other crops were also reported on the Yucatán Peninsula. [20]
President Felipe Calderón cut short a visit to Canada to return to Mexico and assess the damage. [6] Hurricane Dean's Category 5 landfall–the first such landfall in the Atlantic basin in 15 years–took no lives. International organizations,including the United Nations,attributed this to the government's thorough preparations and forecasters' ample warning. [1] [22] [23]
The next day,at 1630 UTC on August 22,Hurricane Dean made a second landfall,this time near the town of Tecolutla,Veracruz,as a Category 2 hurricane. [1] Following the second landfall on the Veracruz coast,the town of Joloapan then saw the eye pass directly over it. In addition,two rivers in the mountains of the state of Hidalgo overflowed,and rain fell as far west as the Pacific coast. Veracruz Governor Fidel Herrera said there was "a tremendous amount of damage". [24] Petroleum production was not severely damaged [25] and quickly returned to normal,although its brief interruption was responsible for a 6% year-on-year decrease in third quarter. [26]
Most intense landfalling Atlantic hurricanes Intensity is measured solely by central pressure | |||
---|---|---|---|
Rank | Hurricane | Season | Landfall pressure |
1 | "Labor Day" [nb 1] | 1935 | 892 mbar (hPa) |
2 | Camille | 1969 | 900 mbar (hPa) |
Gilbert | 1988 | ||
4 | Dean | 2007 | 905 mbar (hPa) |
5 | "Cuba" | 1924 | 910 mbar (hPa) |
Dorian | 2019 | ||
7 | Janet | 1955 | 914 mbar (hPa) |
Irma | 2017 | ||
9 | "Cuba" | 1932 | 918 mbar (hPa) |
10 | Michael | 2018 | 919 mbar (hPa) |
Sources:HURDAT, [28] AOML/HRD, [29] NHC [30] |
Hurricane Dean,at its second landfall,dropped 4 to 8 in (100 to 200 mm) of rainfall across the western states of Jalisco and Nayarit. [31] This rainfall triggered a mudslide in Jalisco which fell on 10 houses and killed one of the occupants. [32] Landslides in Puebla killed five people,and another was crushed when a wall in his house collapsed. One person in Veracruz was electrocuted after touching a power line while repairing his roof. In Michoacán,as the outer bands of the storm swept over the state,a man sheltering under a tree was struck by lightning. [25] [33] Two women died in Hidalgo when heavy rain collapsed their house's roof. [25] [33] [34] Another man drowned while trying to cross a rain-swollen river in Tlacolula,Oaxaca. [34] The heavy rains caused dozens of smaller landslides throughout the country,particularly in Veracruz and Tabasco,but most of them caused no fatalities. [34] At least 50,000 houses were damaged to varying degrees throughout the country. [35] Although Dean's rains caused flooding as far inland as Mexico City,where they closed a portion of Puebla-Mexico highway, [34] the damage was concentrated in the states of Quintana Roo and Veracruz. [35]
As with its first landfall,Hurricane Dean damaged crops throughout its impact area. In Puebla it destroyed 135,000 hectares (330,000 acres) of corn and more than 22,000 hectares (54,000 acres) of coffee,while in Veracruz 15,000 hectares (37,000 acres) of various crops were lost. Unlike in Belize and the Eastern Caribbean,the storm spared the sugarcane crop in Veracruz. [20]
Between the hurricane's two landfalls,Dean affected an estimated 207,800 people in the states of Quintana Roo,Campeche,Veracruz,Hildalgo,Puebla and Tabasco. [35] The storm damaged 85 miles (137 km) of power lines and left more than 100,000 people without electricity. [36] Landslides,storm tides,and widespread structural damage combined to compromise water sources throughout the country. The extent of the damage was never calculated at a federal level,but hundreds of villages lost access to fresh water in the days following the storm. [36] [37] Hurricane Dean killed 12 people in Mexico but none of the deaths occurred during its first and most powerful landfall on the Yucatán Peninsula. [1] Between the two landfalls the storm caused a total of Mex$2 billion (US$184 million) of damages. [38]
Post-storm analysis showed that,while less deadly,Dean's first and more powerful landfall caused significantly more infrastructural damage than its second. Where the landfall occurred at the town of Majahual specifically,and the state of Quintana Roo generally,communities took longer to recover than in the rest of the country. [1] Quintana Roo Governor Félix González Canto reported that although the cleanup in the state capital of Chetumal was completed within three weeks,it took more than six months to fix all of the region's rural roads. [21] Unable to handle the hurricane's aftermath,the state government appealed to federal authorities and secured Mex$755 million (US$74.8 million) of aid. Combined with the state's contribution of $270 million (US$26.7 million),a housing-repair fund of over $1,025 million (US$101.5 million) was established. In the three months immediately following the storm,over 37,000 houses were rebuilt or repaired using monies from this fund. [36]
In the days following the hurricane,immediate access to clean water was a priority for international aid agencies working in Mexico. [12] The National Commission of Water spent another $25 million (US$2.47 million) of federal funds repairing the damaged infrastructure for irrigation and drinking water. [36]
Carnival Cruise Lines and Royal Caribbean Cruises,the world's two largest cuise operators,diverted their ships away from the damaged cruise port of Puerto Costa Maya. Their plans originally expected diversions until at least 2009, [39] but the central government was quick to fund rebuilding of the destroyed concrete piers. By June 2008 they were rebuilt to accommodate even larger ships than before,and ships scheduled stops there for September 2008. [40]
The federal government was initially lauded for its swift and thorough preparation to which most observers,including the United Nations,attributed Dean's low death toll. [22] [23] However,after the storm there were several accusations of political motivation in the distribution of aid. Members of President Felipe Calderón's Partido Accion Nacional (PAN) distributed bags of bread,funded by the nation's disaster relief coffers,carrying the party's logo. In Veracruz Governor Fidel Herrera was accused by both the PAN and his own Partido Revolucionario Institucional (PRI) of using state resources,including hurricane relief,to support the campaigns of PRI candidates. [20]
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 Janet was the most powerful tropical cyclone of the 1955 Atlantic hurricane season and one of the strongest Atlantic hurricanes on record. Janet was also the first named storm to have 1,000 deaths and the first Category 5 storm name to be retired. The eleventh tropical storm, ninth hurricane, and fourth major hurricane of the year, Janet formed from a tropical wave east of the Lesser Antilles on September 21. Moving westward across the Caribbean Sea, Janet fluctuated in intensity, but generally strengthened before reaching its peak intensity as a Category 5 hurricane with winds of 175 mph (282 km/h). The intense hurricane later made landfall at that intensity near Chetumal, Mexico on September 28. After weakening over the Yucatán Peninsula, it moved into the Bay of Campeche, where it slightly strengthened before making its final landfall near Veracruz on September 29. Janet quickly weakened over Mexico's mountainous terrain before dissipating on September 30.
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.
The 1931 Atlantic hurricane season was an active hurricane season, with a total of 13 storms recorded, which was the most since 1916. However, only three of them intensified into hurricanes and just one reached major hurricane intensity, which is Category 3 or higher on the modern-day Saffir–Simpson scale. Nine of the tropical cyclones were identified in real-time, while evidence of the existence of four other tropical cyclones was uncovered by the Atlantic hurricane reanalysis project in 2012 and added to the Atlantic hurricane database. Additionally, two of the tropical storms were upgraded to hurricane status as part of the reanalysis.
Hurricane Claudette was a moderately strong tropical cyclone that struck South Texas in July 2003. A fairly long-lived July Atlantic hurricane, Claudette was the fourth depression, third tropical storm and first hurricane of the 2003 Atlantic hurricane season. Claudette began as a tropical wave in the eastern Caribbean. It moved quickly westward, brushing past the Yucatán Peninsula before moving northwestward through the Gulf of Mexico. Claudette remained a tropical storm until just before making landfall in Port O'Connor, Texas, when it quickly strengthened to a strong Category 1 hurricane on the Saffir-Simpson Hurricane Scale. Forecasting of its path and intensity was uncertain throughout its lifetime, resulting in widespread and often unnecessary preparations along its path.
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.
Hurricane Dolly caused flooding throughout Mexico in August 1996. The fourth named storm and third hurricane of the season, Dolly developed from a tropical wave to the west-southwest of Jamaica on August 19. Initially a tropical depression, the system strengthened into a tropical storm about twelve hours later. Dolly headed westward and intensified into a Category 1 hurricane late on August 20. It then made landfall near Chetumal, Quintana Roo. The system weakened to a tropical depression on August 21. Later that day or early on August 22, Dolly emerged into the Bay of Campeche and quickly re-strengthened into a tropical storm. The storm deepened further and was upgraded to a hurricane again by midday on August 23; Dolly simultaneously peaked with winds of 80 mph (130 km/h). Around that time, it struck between Tuxpan, Veracruz, and Tampico, Tamaulipas. Dolly quickly weakened to a tropical depression early on August 24, but remained intact while crossing Mexico and dissipated over the eastern Pacific Ocean on August 25.
Tropical Storm Chantal was a North Atlantic tropical cyclone that moved across the Caribbean Sea in August 2001. The fourth depression and third named storm of the 2001 Atlantic hurricane season, Chantal developed from a tropical wave on August 14 in the tropical Atlantic Ocean. It tracked rapidly westward for much of its duration, and after degenerating into a tropical wave, it passed through the Windward Islands. Chantal reached a peak intensity of 70 mph (110 km/h) twice in the Caribbean Sea, and each time it was anticipated to attain hurricane status; however, wind shear and later land interaction prevented strengthening to hurricane status. On August 21 Chantal, moved ashore near the border of Mexico and Belize, before dissipating on the next day.
Hurricane Dean was the strongest tropical cyclone of the 2007 Atlantic hurricane season. It was the most intense North Atlantic hurricane since Hurricane Wilma of 2005, tying for eighth overall. Additionally, it made the fourth most intense Atlantic hurricane landfall. A Cape Verde hurricane that formed on August 13, 2007, Dean took a west-northwest path from the eastern Atlantic Ocean through the Saint Lucia Channel and into the Caribbean. It strengthened into a major hurricane, reaching Category 5 status on the Saffir–Simpson hurricane wind scale before passing just south of Jamaica on August 20. The storm made landfall on the Yucatán Peninsula on August 21 at peak intensity. It crossed the peninsula and emerged into the Bay of Campeche weakened, but still remained a hurricane. It strengthened briefly before making a second landfall near Tecolutla in the Mexican state of Veracruz on August 22. Dean drifted to the northwest, weakening into a remnant low which dissipated uneventfully over the southwestern United States. Dean was the second-most intense tropical cyclone worldwide of 2007 in terms of pressure, only behind Cyclone George in the Australian region, and tied with Felix as the most intense worldwide in terms of 1-minute sustained winds.
The meteorological history of Hurricane Dean began in the second week of August 2007 when a vigorous tropical wave moved off the west coast of Africa into the North Atlantic ocean. Although the wave initially experienced strong easterly wind shear, it quickly moved into an environment better suited for tropical development and gained organization. On the morning of August 13, the National Hurricane Center recognized the system's organization and designated it Tropical Depression Four while it was still more than 1,500 mi (2,400 km) east of the Lesser Antilles.
Tropical Storm Arthur was the first Atlantic tropical storm that formed during the month of May since 1981. The first tropical cyclone of the 2008 Atlantic hurricane season, the storm formed on May 30, 2008 from the interaction of two tropical waves and the remnants of the eastern Pacific Tropical Storm Alma, which had crossed into the western Caribbean Sea. The system quickly organized and was named Tropical Storm Arthur on May 31, while crossing the shore of Belize. It dissipated two days later over the Yucatán Peninsula in Mexico. Arthur and its remnants triggered severe flooding which killed a reported nine people and affected 100,000 more in Belize. Damage was light to moderate, estimated at $78 million (2008 USD).
Hurricane Dolly was a strong tropical cyclone that made landfall in Deep South Texas in July 2008. Dolly was the fourth tropical cyclone and second hurricane to form during the 2008 Atlantic hurricane season. Dolly developed on July 20 from an area of disturbed weather in association with a strong tropical wave. It was named at the same time it formed, as the precursor wave already had tropical storm-force winds. This marked the earliest time a fourth named cyclone formed since the 2005 season, which used to hold the record until it was surpassed by the 2012 season, the 2016 season, and the 2020 season.
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.
Hurricane Karl was the most destructive tropical cyclone on record to strike the Mexican state of Veracruz. The eleventh tropical storm, sixth hurricane, and fifth and final major hurricane of the 2010 Atlantic hurricane season, Karl formed from an area of low pressure which had formed off of the northern coast Venezuela on September 11. It crossed the Caribbean and was upgraded to Tropical Storm Karl on September 14. The cyclone made landfall on the Yucatan Peninsula of Mexico as a strong tropical storm, and then rapidly strengthened in the Bay of Campeche before it made landfall near the city of Veracruz, on the central Mexican Gulf coast, as a major hurricane. This marked the first known time that a major hurricane existed in the Bay of Campeche. Afterwards, the storm rapidly weakened over the mountains of Mexico and dissipated on September 18.
Hurricane Ernesto was a Category 2 hurricane and a damaging tropical cyclone that affected several Caribbean Islands and areas of Central America during August 2012. The fifth named storm and second hurricane of the 2012 Atlantic hurricane season, Ernesto originated from a tropical wave that emerged off the west coast of Africa in late July. Moving westward, the system developed into a tropical depression in the central Atlantic, and further into a tropical storm prior to entering the Caribbean Sea. The system encountered high wind shear south of Jamaica but subsequently reached its peak intensity as a Category 2 hurricane as it made landfall on the Yucatán Peninsula. Ernesto briefly emerged in the Bay of Campeche as a strong tropical storm before dissipating over the mountainous terrain of Mexico. The remnant circulation emerged in the eastern Pacific basin, contributing to the formation of Tropical Storm Hector.
The 1942 Belize hurricane was one of only two known hurricanes to strike Belize in the month of November, alongside Hurricane Lisa in 2022. The thirteenth observed tropical cyclone, eleventh tropical storm, and fourth hurricane of the 1942 Atlantic hurricane season, this storm was detected in the vicinity of Turks and Caicos Islands on November 5. Initially a tropical storm, it strengthened slowly while moving westward and then south-southwestward across the Bahamas. On November 6, the storm became a Category 1 hurricane on the modern day Saffir–Simpson hurricane wind scale. Later that day, it made landfall in Cayo Romano, Camagüey Province, Cuba. Impact in Cuba and the Bahamas was limited to lower barometric pressure readings and strong winds. While crossing Cuba, the system weakened to a tropical storm early on November 7, shortly before emerging into the Caribbean Sea. The storm re-strengthened into a hurricane later that day and headed southwestward.
Hurricane Franklin was the first hurricane to make landfall in the Mexican state of Veracruz since Hurricane Karl in 2010. The sixth named storm, first hurricane and the first of ten consecutive hurricanes of the 2017 Atlantic hurricane season, Franklin formed on August 7 out of a tropical wave that was first tracked in the southeastern Caribbean Sea on August 3. The storm strengthened within a favorable environment and made landfall on the Yucatán Peninsula as a moderate tropical storm early on August 8 north of Belize. Weakening occurred as it crossed the peninsula, but Franklin re-emerged into the Bay of Campeche later that day, restrengthening quickly to become the season's first hurricane. It made landfall near Lechuguillas, Veracruz, on August 10 as a Category 1 hurricane, before rapidly weakening over the mountainous terrain of Mexico and dissipating shortly afterwards. On August 12, the storm's remnant mid-level circulation combined with a developing low in the Eastern Pacific to form Tropical Storm Jova.
The effects of Hurricane Wilma in Mexico severely affected the tourism industry of the Yucatán Peninsula in mid October 2005. Hurricane Wilma developed on October 15 in the Caribbean. Four days later, it intensified into the strongest Atlantic hurricane on record as determined by barometric pressure. Wilma weakened as it moved slowly northwestward, eventually making landfall late on October 21 on the island of Cozumel. At the time, it was a Category 4 hurricane on the Saffir–Simpson scale. Early the next day, the hurricane made another landfall on the Mexican mainland near Puerto Morelos. Wilma exited the Yucatán Peninsula into the Gulf of Mexico on October 23, and a day later it struck Florida.
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.