Meteorological history | |
---|---|
Formed | September 14,2010 |
Dissipated | September 18,2010 |
Category 3 major hurricane | |
1-minute sustained (SSHWS/NWS) | |
Highest winds | 125 mph (205 km/h) |
Lowest pressure | 956 mbar (hPa);28.23 inHg |
Overall effects | |
Fatalities | 22 total |
Damage | $3.9 billion (2010 USD) |
Areas affected | Belize,Yucatán Peninsula,Veracruz |
IBTrACS | |
Part of the 2010 Atlantic hurricane season |
Hurricane Karl was the most destructive tropical cyclone on record to strike the Mexican state of Veracruz. [1] 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 of 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.
At least 22 people were confirmed dead,most of which were in the state of Veracruz. [2] Insured losses from the storm were estimated to be US$206 million,with total economic losses of approximately $3.9 billion. [3]
The origins of Hurricane Karl were from the interaction between a surface trough and westward-tracking tropical wave. The trough—an elongated area of low pressure—emerged from an area of disorganized monsoonal convection just north of South America over the Windward Islands in early September. [4] [5] A few days later, the wave, which had departed the coast of Africa on September 1, approached the area and merged with the trough by September 8 as it slowed. [6] For several days, the resultant low-pressure system lingered toward the west-northwest over the Caribbean Sea, and provided with a diffluent environment aloft it generated disorganized patches of convection. [7] [8] Although the convection remained disassociated from the mean low feature, the overall wind circulation continued to become better defined at the surface. The development trend briefly became disrupted by September 13, however, with the surface low confirmed no longer to exist under the improving convective structure. [6] Conditions remained favorable for reorganization, and a small but consolidated circulation center developed by 2100 UTC September 14. [9] In real time, this marked the formation of Tropical Storm Karl when it was located about 270 mi (435 km) east of Chetumal, Mexico, though post-storm reanalysis revealed a tropical depression had in fact formed six hours earlier. [6] [10]
With a predominant ridge anchored to its north along the Gulf of Mexico, Karl continued a generally westward motion for most of its duration. Supported by symmetrical upper-level outflow, the storm strengthened slowly over very high water temperatures in a low-shear environment. [11] [12] Karl subsequently made its initial landfall on the southeastern coast of Yucatán as a strong tropical storm early on September 15, with estimated winds of 65 mph (100 km/h). As it moved inland, radar imagery from Belize depicted a developing eye, suggesting the storm might have reached hurricane status at the time. [13] Although the storm slowly weakened as it crossed the Yucatán, its cloud pattern remained well-organized, with a ring of deep convection surrounding an eye-like feature. [14] Around 0400 UTC September 16, the center of Karl emerged into the Bay of Campeche as it slowed slightly. Situated once again over warm waters in a favorable shear environment, Karl steadily intensified and reached hurricane status about 150 mi (240 km) off the coast of Campeche, Mexico, after reconnaissance found a developing eyewall. At the time, Karl co-existed with hurricanes Igor and Julia, the first such occasion since 1998 with at least three simultaneous hurricanes in the North Atlantic. [15]
The hurricane entered a period of rapid intensification after steadily deepening for several hours; its cloud pattern quickly organized, and with cooling convective cloudtops the warm eye became well-defined. [16] Recurving toward the southwest along the building ridge, Karl became a Category 3 hurricane on September 17; it reached its peak intensity of 125 mph (205 km/h) only four hours prior to landfall. [17] Karl became the strongest hurricane ever observed in the Bay of Campeche upon attaining this intensity, a record previously set by Hurricane Item in 1950, [6] – later to be tied by Hurricane Grace in 2021. Despite a sudden increase in minimum central pressure, Karl retained its strength and moved ashore near Veracruz, Mexico as a major hurricane at 16:45 UTC. [6] Once inland, the small storm rapidly weakened over the high terrain, and by early September 18 no deep convection remained around its increasingly disrupted circulation. [18] Around 0900 UTC, the system was declassified as a tropical cyclone as its low-level circulation dissipated, though patches of remnant thunderstorms continued to produce heavy precipitation over the country. [19]
Upon the formation of a tropical cyclone, the government of Mexico issued a tropical storm warning for the east coast of the Yucatán Peninsula, extending from Chetumal northward to Cabo Catoche. Additionally, a tropical storm watch was in place for the coast of northern Belize, from Belize City to the Belize–Mexico border. [10] At the threat of a storm, authorities in Honduras declared a green alert for the entire country; a yellow alert was to remain in effect for 36 hours in the Bay Islands Department. [20] [lower-alpha 1] El Cajón, a major hydroelectric power plant located in western Honduras, discharged some of its water reservoir into connecting rivers to prevent flooding of surrounding low-lying areas. Port officials along the coastlines were advised to take necessary precautions due to rough sea conditions. [21] In Belize, seaports secured their supplies and halted operations to ensure the safety of seafaring vessels and marine workers. [22] Schools were closed in the northern districts of Corozal and Orange Walk, as well as in San Pedro Town and Caye Caulker during the storm's passage. [23]
In Quintana Roo, officials opened shelters and ordered the evacuation of low-lying areas along the storm's projected path. Hundreds of people were displaced at Banco Chinchorro, an atoll reef and diving center near Majahual. In Carillo Puerto, located to the south of the archaeological ruins of Tulum, authorities readied concrete residences to provide shelter to some hundred communities of indigenous Mayans. [24] As Karl moved further inland, orange alerts were declared in Campeche for the municipalities of Hopelchén and Calakmul, while the rest of the state remained under yellow alert. [25] Shelters were opened near flood-prone areas in the cities of Campeche, Champotón and the municipality of Calkiní (Isla Arena). Local residents were urged not to take out their trash for three days, as collection services were to be suspended at the threat of torrential rainfall. [26]
The government of the Veracruz issued a red alert as Karl approached the state's coastline; eight municipalities were placed under mandatory coastal evacuation orders. Laguna Verde Nuclear Power Station, located in the Veracruz coastline, stopped its operations as a precaution. Additionally, Pemex evacuated its facilities on the Gulf of Mexico that were located in Karl's path. [27] World oil prices rose rapidly on September 17 as the company stopped production on 14 of its wells. The prices climbed 54 cents to 75.11 dollars a barrel. [28]
As Karl struck the coast of Quintana Roo, heavy precipitation amounting up to 6.2 inches (157 mm) in some areas resulted in scattered flooding. [29] At the height of the storm, a total of 54,265 residents were without power, but most had their electricity restored within a day. [30] Some 600 homes in Chetumal suffered inundations of up to 4.9 ft (1.5 m), forcing hundreds of residents to evacuate. [29] [31] High winds reportedly uprooted several trees in Bacalar, a small village near the city. [24] The municipalities of Othon P. Blanco, Carillo Puerto, and José María Morelos reported copious losses in agriculture; an estimated total of 11,650 hectares of crop were affected, with 3,477 hectares of maiz crop destroyed. Approximately 7,800 hectares of sugarcane along the banks of the Hondo River were lost, resulting in economic losses of Mex$76 million (US$6.23 million). [32] In Othon P. Blanco, 477 hectares of jalapeño chili peppers were lost while banana, cassava and citrus plantations in the area sustained significant wind damage. [33] In total, damage to roads, structures and properties in the municipality was estimated at Mex$120 million (US$9.9 million). [34]
Though there were no reports of major damage, strong winds in Belize downed utility poles, grounded water crafts and caused power outages along the Belize–Mexico border. [23] Further inland in Campeche, maximum 24-hour rainfall accumulations totaled no more than 0.95 inches (24 mm), and little damage was reported. [25] [35] The storm left no fatalities in its wake in the peninsula, as its landfall occurred in a sparsely populated area. [36]
Succeeding one of Mexico's wettest seasons on record, torrential rains from Karl brought on historic flooding that lead to great destruction across Veracruz. [37] The heaviest precipitation occurred adjacent to and northward of the storm's track, with localized accumulations of up to 17.83 inches (455 mm) recorded in Misantla. On landfall, major-hurricane-force winds uprooted hundred thousands of trees and caused widespread power outages, leaving up to 280,000 customers in the dark. [38] The disaster affected at least 163 of the state's 212 municipalities, and several days after its passage more than half of the territory remained submerged by the flood waters. [39] [37] It caused the largest population displacement in the region's history; about 150,000 residents evacuated to a total of 423 storm shelters statewide. [40] Karl claimed the lives of a confirmed twelve people in the state, [41] [42] among which a 40-year-old woman, along with her two- and three-year-old grandchildren in Cotaxtla, and a 54-year-old and an 87-year-old in Felipe Carrillo. [43] Two other fatalities were however mentioned as being possibly attributed to the storm in an official government press release on September 24, 2010. [41]
In addition to the loss of life, structural damage in the state was widespread and particularly severe. In Cotaxtla, damaging muddy waters up to 12 m (39 ft) high left much of the municipality inundated and scores structures encased in mud. In some areas, the flooding was described as being "unprecedented". [44] Carrillo Puerto suffered similar damage; two people were reported missing in the city. [45] The impact on the vegetation was particularly notable in Boca del Río —situated near the mouth of the Jamapa River —where the winds downed well over 400,000 trees; [46] a consequent clogging of the river mouth prompted about 30,000 people to evacuate from adjacent areas. [47] In Puebla, two people were killed after their home was destroyed in a landslide. [48] A third person was killed in Tabasco after she drowned in her flooded home. [49] An estimated 200,000 residences were left without power as a result of Karl. [50]
In total, Karl killed 16 people and left 11 others missing. [45] [51] [52] An estimated 15.8 million people were affected by the storm throughout Mexico. [53] Preliminary assessments placed the damage from Karl in Veracruz at 70 billion MXN (US$5.6 billion). [54] [55] In Puebla, losses from the storm reached 200 million MXN (US$16 million). [56] Final estimates of economic losses throughout Mexico total MXN50 billion (US$3.9 billion), with insured losses at MXN2.5 billion (US$200 million). [3]
Following severe flooding triggered by Karl, roughly 3,500 people sought refuge in shelters set up at schools throughout Veracruz. Between 250,000 and 500,000 people are believed to have been left homeless as 120 municipalities throughout the state experience extensive floods. Emergency officials stated that all warnings would remain in place despite Karl having already passed to keep the public informed of lingering danger. [45] In the weeks following the hurricane, recovery crews cleared roughly 18,000 tonnes of debris throughout the state of Veracruz. [57]
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 Gert was a large tropical cyclone that caused extensive flooding and mudslides throughout Central America and Mexico in September 1993. The seventh named storm and third hurricane of the annual hurricane season, Gert originated as a tropical depression from a tropical wave over the southwestern Caribbean Sea on September 14. The next day, the cyclone briefly attained tropical storm strength before moving ashore in Nicaragua and proceeding through Honduras. It reorganized into a tropical storm over the Gulf of Honduras on September 17, but weakened back to a depression upon crossing the Yucatán Peninsula. Once over the warm waters of the Bay of Campeche, Gert quickly strengthened into a Category 2 hurricane by September 20. The hurricane made a final landfall on the Gulf Coast of Mexico near Tuxpan, Veracruz, with peak winds of 100 mph (160 km/h). The rugged terrain disrupted the cyclone's structure; Gert entered the Pacific Ocean as a depression near the state of Nayarit on September 21, where it briefly redeveloped a few strong thunderstorms before dissipating at sea five days later.
Tropical Storm Bret was a short-lived tropical storm in June 2005 that had damaging effects in Veracruz, Mexico. The second named storm of the season, Bret quickly developed from a tropical wave on June 28 in the Bay of Campeche. Failing to intensify beyond minimal tropical storm intensity, the system made landfall in Veracruz the following day. It rapidly weakened once onshore, dissipating early on June 30. The storm brought heavy rainfall to Veracruz, San Luis Potosí, and Tamaulipas with the former suffering the brunt of the impacts. Approximately 11,000 people were adversely affected by widespread flooding. A total of 2,129 homes were damaged and 25 were destroyed, mostly in the city of Naranjos. Three people were killed in storm-related incidents and total losses exceeded 100 million pesos (US$9.3 million). The Government of Veracruz declared emergencies for nine municipalities and released tens of millions of pesos in relief aid in conjunction with national agencies.
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 Lorenzo was a rapidly developing tropical cyclone that struck the Mexican state of Veracruz in late September 2007. The twelfth named storm and fifth hurricane of the 2007 Atlantic hurricane season, it formed in the southwestern Gulf of Mexico from a tropical wave. After meandering for two days without development, the storm began a steady westward track as its structure became better organized. In an 18‑hour period, Lorenzo's winds increased from 35 mph (55 km/h) to 80 mph (130 km/h), or from a tropical depression to a hurricane. On September 28 it struck near Tecolutla, Veracruz, a month after Hurricane Dean affected the same area, before it quickly dissipated over land.
Tropical Storm Marco was one of the smallest tropical cyclones on record by radius of winds from center. The thirteenth named storm of the 2008 Atlantic hurricane season, Marco developed out of a broad area of low pressure over the northwestern Caribbean during late September 2008. Influenced by a tropical wave on October 4, a small low-level circulation center developed over Belize. After crossing the southern end of the Yucatán Peninsula and emerging into the Bay of Campeche, the low was declared Tropical Depression Thirteen early on October 6. The depression quickly intensified into a tropical storm and was given the name Marco later that day. Marco reached its peak intensity with winds of 65 mph (100 km/h) early on October 7. Around this time, tropical storm force winds extended 11.5 miles (18.5 km) from the center of the storm, making Marco the smallest tropical cyclone on record. Around 1200 UTC, Marco made landfall near Misantla, Veracruz. The storm rapidly weakened after landfall, dissipating later that day.
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.
Hurricane Alex was the first tropical cyclone of the 2010 Atlantic hurricane season, and a rare June Atlantic hurricane. Originating from an area of disturbed weather on June 25, 2010, it slowly developed in the western Caribbean Sea and struck Belize as a strong tropical storm. After entering the Gulf of Mexico, Alex became very large and encountered conditions favorable for gradual development. Early on June 30, the cyclone attained hurricane status as it approached northeastern Mexico, the first June hurricane in the Atlantic basin since Hurricane Allison in 1995, and the storm rapidly intensified just off the coast of Tamaulipas. Alex made landfall near Soto la Marina as a Category 2 hurricane on the Saffir-Simpson Hurricane Wind Scale. Alex rapidly weakened after landfall, with the storm losing its tropical status on July 2, before fully dissipating on July 6.
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.
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.
Tropical Storm Barry was a weak and short-lived tropical cyclone that brought heavy rains to parts of Central America and Mexico in June 2013. Barry originated from a tropical wave that developed in the southern Caribbean Sea. The wave tracked northwestward and began to develop in marginally favorable conditions. On June 17, the disturbance was upgraded to Tropical Depression Two by the National Hurricane Center. Due to its close proximity to land, the system failed to intensify before crossing the southern Yucatán Peninsula. The depression emerged over the Bay of Campeche late on June 18 and became increasingly organized. During the afternoon of June 19, data from Hurricane Hunters revealed the system had intensified into a tropical storm. The newly named Barry attained peak winds of 45 mph (75 km/h) before making landfall in Veracruz, Mexico on June 20. Once onshore, the storm quickly weakened and degenerated into a remnant low that night.
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 Dolly was a short-lived and disorganized tropical cyclone that caused moderate damage across Tamaulipas, Mexico, in early September 2014. Originating from a tropical wave, the system first became a tropical depression late on September 1 while situated over the Bay of Campeche. Dolly struggled against strong wind shear for the duration of its existence. The large system featured multiple circulations, sometimes becoming a new dominant center and other times simply rotating around a mean vortex. As a result, multiple center relocations occurred along its general west-northwest track. Dolly eventually made landfall in Tamaulipas on September 3 before degenerating into a remnant low. The system subsequently dissipated the following day.
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 Earl was the deadliest Atlantic hurricane to impact Mexico since Hurricane Stan in 2005. The fifth named storm and second hurricane of the 2016 Atlantic hurricane season, Earl formed from a tropical wave south of Jamaica on August 2. The precursor to Earl brought torrential rainfall and flooding to the Lesser Antilles. Upon classification, the storm moved westward through the Caribbean Sea, brushing the north coast of Honduras. Earl strengthened into an 85 mph (140 km/h) hurricane before making landfall on Belize on August 4. It weakened while moving across the Yucatán Peninsula, but reintensified in the Bay of Campeche and followed the coastline. On August 6, Earl dissipated after moving ashore Veracruz.
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 Vicente was an unusually small tropical cyclone that made landfall as a tropical depression in the Mexican state of Michoacán on October 23, 2018, causing deadly mudslides. The 21st named storm of the 2018 Pacific hurricane season, Vicente originated from a tropical wave that departed from Africa's western coast on October 6. The wave traveled westward across the Atlantic and entered the Eastern Pacific on October 17. The disturbance became better defined over the next couple of days, forming into a tropical depression early on October 19. Located in an environment favorable for further development, the system organized into Tropical Storm Vicente later that day.
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.
Tropical Storm Dolores was a strong tropical storm that made landfall in southwestern Mexico in June 2021. The fourth named storm of the 2021 Pacific hurricane season, Dolores developed from a low-pressure area that formed offshore the Mexican state of Oaxaca on June 16, 2021. The low steadily developed organized deep convection and a closed surface circulation, becoming Tropical Depression Four-E around 06:00 UTC June 18. The depression strengthened into a tropical storm nine hours later and was named Dolores. Gradually approaching the southwestern coast of Mexico, Dolores steadily intensified despite its close proximity to land. The storm reached its peak intensity around 15:00 UTC June 19 with maximum sustained winds of 115 km/h (70 mph) and a minimum barometric pressure of 29.2 inHg (989 mbar), just below hurricane strength. Shortly after reaching this intensity, Dolores made landfall just northwest of Punta San Telmo, near the Colima–Michoacán state border. The storm rapidly weakened as it moved inland over Mexico and dissipated early on June 20 over the state of Zacatecas.