Meteorological history | |
---|---|
Formed | October 3,2023 |
Dissipated | October 11,2023 |
Category 4 major hurricane | |
1-minute sustained (SSHWS/NWS) | |
Highest winds | 140 mph (220 km/h) |
Lowest pressure | 942 mbar (hPa);27.82 inHg |
Overall effects | |
Fatalities | 3 |
Damage | $77.6 million (2023 USD) |
Areas affected | Western Mexico,Islas Marías,Southwestern Mexico,Texas |
IBTrACS / [1] [2] | |
Part of the 2023 Pacific hurricane season |
Hurricane Lidia was a powerful Category 4 Pacific hurricane that was one of four tropical cyclones to make landfall on the Pacific Coast of Mexico in October 2023. The fifteenth tropical depression,twelfth named storm,eighth hurricane and sixth major hurricane [lower-alpha 1] of the 2023 Pacific hurricane season,Lidia originated from a disturbance that developed to the south of Mexico in late September 2023. The disturbance developed into a tropical storm on October 3,and was given the name Lidia. Lidia initially meandered off the coast of Mexico for several days as a moderate tropical storm,while moving gradually northward. Lidia first turned northwestward before embarking on a northeastward course on October 9,at which time the storm began a phase of rapid intensification. Early on October 10,Lidia became a hurricane,and the storm continued to quickly intensify,reaching its peak intensity as a Category 4 hurricane late that day with sustained winds of 140 mph (220 km/h). Lidia made landfall shortly afterwards at peak intensity,making it the third-strongest landfalling Pacific hurricane on record at the time. Lidia rapidly weakened over the mountainous terrain of Mexico and dissipated the following morning over the inland state of Zacatecas.
Lidia caused extensive damage across southwestern Mexico,impacting the area less than 48 hours after it was struck by Tropical Storm Max. Lidia resulted in significant flooding,torrential rainfall and very powerful winds that severely damaged many structures,and the storm forced airport and school closings,along with the opening of 23 temporary shelters. Three deaths occurred due to Lidia in Mexico. Enrique Alfaro,the governor of Jalisco,estimated that losses from Lidia in the state totaled MXN$1.4 billion (USD$77.6 million). [lower-alpha 2]
As early as September 28, the National Hurricane Center (NHC) anticipated that a low pressure area would form south of Mexico, assessing a 20% chance of tropical cyclogenesis within seven days. [3] Two days later, the NHC increased the potential for development to 70% – this was related to a tropical wave south of Mexico producing an area of thunderstorms, known as convection. [4] On October 2, the convection became more concentrated, supported by favorable environmental conditions, and a low pressure area developed. [5] [6] At 09:00 UTC on October 3, the NHC initiated advisories on Tropical Storm Lidia, due to sufficient organization of the weather system. By that time, the thunderstorms had organized into curved rainbands, and the low pressure area had evolved into a well-defined circulation producing sustained winds of at least 40 mph (65 km/h). [7]
Upon its formation, Lidia was expected to intensify to hurricane status within five days, due to sea surface temperatures of around 86 °F (30 °C) and ample moisture. [7] However, the presence of easterly wind shear was an early deterring factor, which displaced the convection from the center. [8] The thunderstorms continued to pulse over the center as Lidia moved north-northwestward, a path steered by a ridge over Mexico. Despite the wind shear, Lidia was able to continue to intensify. [9] By October 6, the storm turned toward the west, as the circulation become more closely aligned with the deepest convection, a sign of a maturing tropical cyclone. [10] Later that day, the wind shear nearly exposed the center from the thunderstorms, although the intensity had increased to just below hurricane-force, or winds of 74 mph (118 km/h). By that time, hurricane models had conflicting simulations for the future of Lidia. In the storm's immediate future, there was a consensus that a mid-latitude trough would steer the storm northward. Some computer models anticipated that the wind shear would remain strong enough to weaken the storm, while others predicted that it would intensify while moving toward the western coast of Mexico. [11]
On October 7, Lidia began its anticipated turn to the north. With the wind shear continuing to affect, there was still uncertainty in the storm's future. That day, the NHC forecast included a hurricane landfall in the Mexican state of Nayarit. [12] By October 8, Lidia's structure had become more organized, with the center under the deepest convection, and a mid-level eye forming. [13] The lower- and mid-level circulations were displaced, while the intrusion of drier air prevented more immediate intensification. [14] [15] On October 9, Lidia began its turn to the northeast, influenced by the approaching mid-level trough, which provided more favorable upper-level support. Concurrently, the convection increased over the center, signaling the start of an intensifying trend, which the NHC expected would continue up to the coast. [16]
Late on October 9, the Hurricane Hunters flew into Lidia, observing a developing inner core of the cyclone, with a central barometric pressure of 985 mbar (29.1 inHg). [17] Early on October 10, the storm intensified into a hurricane while located about 365 mi (590 km) southwest of Puerto Vallarta. [18] As Lidia approached the Mexican coast, it developed an eyewall as it intensified into a Category 2 hurricane on the Saffir-Simpson scale. [19] It then rapidly intensified to a Category 4 hurricane by 21:30 UTC on October 10, [20] making landfall two hours later near Las Peñitas in the Mexican state of Jalisco, just south of Puerto Vallarta, at peak intensity, with winds of 140 mph (220 km/h). Once inland, Lidia rapidly weakened over the mountainous terrain of western Mexico. The eye quickly degraded and the convection diminished. [21] By 09:00 UTC on October 11, the storm lost its well-defined center, less than ten hours after landfall. Lidia's remnants continued northeastward across northern Mexico, producing a large area of rainfall. [22]
Hurricane | Season | Wind speed | Ref. |
---|---|---|---|
Otis | 2023 | 160 mph (260 km/h) | [23] |
Patricia | 2015 | 150 mph (240 km/h) | [24] |
Madeline | 1976 | 145 mph (230 km/h) | [25] |
Iniki | 1992 | [26] | |
Twelve | 1957 | 140 mph (220 km/h) | [27] |
"Mexico" | 1959 | [27] | |
Kenna | 2002 | [28] | |
Lidia | 2023 | [29] |
Lidia prompted the issuance of hurricane and tropical storm watches and warnings for western Mexico. [30] Schools were closed across 23 municipalities in Mexico ahead of Lidia's anticipated landfall in the states of Sinaloa, Nayarit, and Jalisco, particularly in the latter state due to the combined threat of Lidia and the more southerly-tracking Tropical Storm Max, which made landfall in Guerrero less than two days prior. [31] [32] 23 storm shelters were opened in Jalisco alone. [33] Several businesses in the resort town of Puerto Vallarta shut down and boarded up windows and doors and used sandbags as flood barriers. [34] Licenciado Gustavo Díaz Ordaz International Airport was also closed on October 11 as Lidia approached the area, and 12 flights were cancelled. [35] 6,000 Mexican armed forces members were deployed to Nayarit and Jalisco by Mexican President Andres Manuel Lopez Obrador to assist residents in vulnerable areas. [32] [36]
At the time of its landfall, Hurricane Lidia was the third-most intense Pacific hurricane on record to make landfall in Mexico. [37] The cyclone produced intense rainfall and flash flooding as it moved onshore and inland over Jalisco. One person was killed in Punta Mita after strong winds from Lidia downed a tree on a van while another drowned in a swollen river. A third death occurred due to a bridge collapse in Villa de Álvarez, Colima. [38] [2] Numerous trees were uprooted, some of which blocked Federal Highway 200, and 136 people were placed in temporary storm shelters due to the hurricane. [39] Several rivers and streams overflowed, which inundated houses and forced the closure of a hospital in Autlán de Navarro. [40] Downed trees and power lines were reported across coastal Jalisco. [41] Lidia significantly disrupted tourism along the coast, with several hotels, beaches and airports shutting down in response to the cyclone. [42] Lidia's powerful winds uprooted nearly 960 trees across Puerto Vallarta; in response, a reforestation drive was initiated by the municipal government in November 2023. [43] Several homes in the city had their rooves blown completely off by Lidia's powerful winds, and two people were seriously injured during the storm. [33] Preliminary rainfall totals reached 5.3 in (130 mm) in the neighboring state of Colima, with 5.1 in (130 mm) falling in the city of Manzanillo. [44]
Jalisco's governor, Enrique Alfaro, estimated that Lidia caused losses worth MXN$1.4 billion (USD$77.6 million) in the state. Alfaro appealed to the Mexican federal government for financial support in recovery efforts from the cyclone. [1] The combined remnant moisture of Lidia and Max combined with a frontal boundary over the Gulf of Mexico and contributed to beneficial rainfall along the Gulf Coast of the United States, which was suffering from drought conditions. [45] Moisture from Lidia's remnants also sent moderate rainfall into southern Texas. [44]
Hurricane Kenna was the fourth-most intense tropical cyclone on record in the Eastern Pacific basin, and at the time the third-most intense Pacific hurricane to strike the west coast of Mexico. Kenna was the sixteenth tropical depression, thirteenth tropical storm, seventh hurricane, sixth major hurricane, and third Category 5 hurricane of the 2002 Pacific hurricane season. After forming on October 22 to the south of Mexico from a tropical wave, forecasters consistently predicted the storm to strengthen much less than it actually did. Moving into an area of favorable upper-level conditions and warm sea surface temperatures, Kenna quickly strengthened to reach peak winds of 165 mph (270 km/h) as a Category 5 hurricane, on October 25, while located about 255 mi (410 km) southwest of Puerto Vallarta, Jalisco. Weakening as it turned to the northeast, the hurricane made landfall near San Blas, Nayarit as a Category 4 hurricane, with sustained winds of 140 mph (220 km/h), before dissipating on October 26 over the Sierra Madre Occidental mountains.
The 2002 Pacific hurricane season was a near–average season which produced fifteen named storms. Eight hurricanes formed, including a record-equaling three Category 5 hurricanes, a record it shares with the 1994 and 2018 seasons. It was also a near-average season in terms of accumulated cyclone energy (ACE), having an ACE of 125. The season officially began on May 15, 2002 in the East Pacific Ocean, and on June 1, 2002 in the Central Pacific; both ended on November 30. These dates conventionally delimit the period of each year when most tropical cyclone formation occurs in these regions of the Pacific. The first system of the 2002 season, Hurricane Alma, formed on May 24, and the last, Tropical Depression Sixteen-E, dissipated on November 16.
The 1998 Pacific hurricane season was a fairly average Pacific hurricane season. Despite this, it had nine hurricanes and six major hurricanes, which was well above average. The season officially started on May 15 in the eastern Pacific and on June 1 in the central Pacific, and ended on November 30; these dates conventionally delimit the period during which most tropical cyclones form in that region. The first tropical cyclone developed on June 11, about ten days later than the normal start of the season. The final storm of the year, Hurricane Madeline, dissipated on October 20. Storm activity in the Central Pacific Hurricane Center's warning zone was low, with just one tropical depression observed in the region. Two tropical cyclones from the eastern Pacific also entered the central Pacific; the former did so as a hurricane.
The 1996 Pacific hurricane season had below normal tropical cyclone activity, producing 9 tropical storms, of which 5 became hurricanes, with 2 of those intensifying into major hurricanes. With an Accumulated cyclone energy (ACE) index of 53.9, the season ranks among the least intense Pacific hurricane seasons on record. It officially began May 15, 1996, in the eastern north Pacific and on June 1, 1996, in the central north Pacific. It ended on November 30, 1996. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. The season slightly exceeded these bounds when tropical storm One-E formed on May 13.
The 2012 Pacific hurricane season was a moderately active Pacific hurricane season that saw an unusually high number of tropical cyclones pass west of the Baja California Peninsula. The season officially began on May 15 in the eastern Pacific Ocean, and on June 1 in the central Pacific (from 140°W to the International Date Line, north of the equator; they both ended on November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in these regions of the Pacific Ocean. However, the formation of tropical cyclones is possible at any time of the year. This season's first system, Tropical Storm Aletta, formed on May 14, and the last, Tropical Storm Rosa, dissipated on November 3.
Tropical Storm Norman was a tropical cyclone that hit Mexico in September 2000. The sixteenth cyclone and fourteenth named storm of the 2000 Pacific hurricane season, Norman originated in a tropical wave that emerged from the coast of Africa on September 4, and moved westward across the Atlantic Ocean; the wave entered the Pacific on September 16. The disturbance organized into a tropical depression on early on September 20, and later that day the storm reached its peak intensity of 50 mph (80 km/h), and subsequently made landfall to the west of Lázaro Cárdenas, Michoacán. After weakening to a tropical depression over land, the storm re-emerged over open waters, and made a second landfall before dissipating shortly thereafter. The storm produced heavy rain that resulted in flooding and mudslides, killing about nine people.
Hurricane Rick was the third-most intense Pacific hurricane on record and the second-most intense tropical cyclone worldwide in 2009, only behind Typhoon Nida. Developing off the southern coast of Mexico on October 15, Rick traversed an area with favorable environmental conditions, favoring rapid intensification, allowing it to become a hurricane within 24 hours of being declared a tropical depression. An eye began to form during the afternoon of October 16; once fully formed, the storm underwent another period of rapid strengthening. During the afternoon of October 17, the storm attained Category 5 status on the Saffir–Simpson hurricane wind scale. Several hours later, Rick attained its peak intensity as the third-strongest Pacific hurricane on record with winds of 180 mph (290 km/h) and a barometric pressure of 906 mbar.
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Hurricane Patricia was the most intense tropical cyclone ever recorded in the Western Hemisphere and the second-most intense worldwide in terms of barometric pressure. It also featured the highest one-minute maximum sustained winds ever recorded in a tropical cyclone. Originating from a sprawling disturbance near the Gulf of Tehuantepec in mid-October 2015, Patricia was first classified a tropical depression on October 20. Initial development was slow, with only modest strengthening within the first day of its classification. The system later became a tropical storm and was named Patricia, the twenty-fourth named storm of the annual hurricane season. Exceptionally favorable environmental conditions fueled explosive intensification on October 22. A well-defined eye developed within an intense central dense overcast and Patricia grew from a tropical storm to a Category 5 hurricane in just 24 hours—a near-record pace. The magnitude of intensification was poorly forecast and both forecast models and meteorologists suffered from record-high prediction errors.
Tropical Storm Lidia was a large tropical cyclone that caused flooding in Baja California Peninsula and parts of western Mexico. The fourteenth tropical cyclone and twelfth named storm of the 2017 Pacific hurricane season, Lidia developed from a large area of disturbed weather west of the Pacific Coast of Mexico on August 31. The storm intensified while moving generally northward or northwestward, peaking with maximum sustained winds of 65 mph (105 km/h) later that day. On September 1, Lidia made landfall in Mexico near Puerto Chale, Baja California Sur, at peak intensity. The storm weakened while traversing the peninsula, ultimately emerging over the Pacific Ocean on September 3, where the storm degenerated into a remnant low. The system brought thunderstorms and wind gusts to Southern California, before dissipating on September 4.
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Hurricane Orlene was a powerful tropical cyclone that caused minor damage to the Pacific coast of Mexico in October 2022. The cyclone was the sixteenth named storm, ninth hurricane, and third major hurricane of the 2022 Pacific hurricane season. Orlene originated from a low-pressure area off the coast of Mexico. Moving towards the north, Orlene gradually strengthened, becoming a hurricane on October 1 and reaching its peak intensity the following day with winds of 130 mph (215 km/h). Orlene made landfall just north of the Nayarit and Sinaloa border, with winds of 85 mph (140 km/h). Soon afterward, Orlene rapidly weakened and became a tropical depression, eventually dissipating over the Sierra Madre Occidental late on October 4.
Hurricane Roslyn was a powerful tropical cyclone that struck the Pacific coast of Mexico in October 2022. The nineteenth named storm, tenth hurricane, and fourth major hurricane of the 2022 Pacific hurricane season, Roslyn formed on October 20, from an area of low pressure that developed off the southwestern coast of Mexico. The system moved west-northwestward, paralleling the coast, where it became a hurricane at 00:00 UTC, on October 22, and, within 18 hours rapidly intensified to a Category 4 hurricane, with sustained winds of 130 mph (215 km/h). Roslyn made landfall on October 23 near Santa Cruz in northern Nayarit, at 11:20 UTC with 120 mph (195 km/h) winds. Inland, Roslyn weakened quickly to a tropical storm, and then dissipated over east-central Mexico on October 24.
This article incorporates public domain material from websites or documents of the National Weather Service .