Meteorological history | |
---|---|
Formed | September 7,2021 |
Remnant low | September 11,2021 |
Dissipated | September 12,2021 |
Category 2 hurricane | |
1-minute sustained (SSHWS/NWS) | |
Highest winds | 105 mph (165 km/h) |
Lowest pressure | 975 mbar (hPa);28.79 inHg |
Overall effects | |
Fatalities | 1 total |
Damage | $19 million |
Areas affected | Western Mexico,Baja California Sur |
IBTrACS / [1] | |
Part of the 2021 Pacific hurricane season |
Hurricane Olaf was a Category 2 Pacific hurricane that struck the Baja California Peninsula in September 2021. The fifteenth named storm and sixth hurricane of the 2021 Pacific hurricane season,the cyclone formed from an area of low pressure that developed off the southwestern coast of Mexico on September 5,2021. The disturbance developed within a favorable environment,acquiring more convection and a closed surface circulation. The disturbance developed into Tropical Depression Fifteen-E by 18:00 UTC [lower-alpha 1] on September 7. The depression strengthened into a tropical storm and was named Olaf at 12:00 UTC the next day. Olaf quickly strengthened as it moved to the north-northwest,and was upgraded to a hurricane 24 hours after being named. Hurricane Olaf continued to intensify and reached peak intensity while its center was just offshore the southwestern coast of Baja California Sur,with maximum sustained winds of 105 mph (169 km/h) and a minimum barometric pressure of 975 mbar (28.8 inHg). Just after reaching peak intensity,the hurricane made landfall near San Josédel Cabo. Interaction with the mountainous terrain of the Baja California Peninsula caused Olaf to quickly weaken. It was downgraded to a tropical storm at 12:00 UTC on September 10. The system became devoid of convection later that day and degenerated to a remnant low by 06:00 UTC on September 11.
The precursor disturbance to Olaf caused flooding in the southwestern Mexican states of Jalisco and Colima. The storm triggered school,port,and COVID-19 vaccination-site closures in Baja California Sur as it approached the peninsula. Severe rainfall,flooding,mudslides,uprooted trees and damage to power lines and hotels affected the state as the hurricane made landfall and moved over the peninsula. Total damage from Olaf was estimated at USD$19 million, [lower-alpha 2] and one person died due to a mudslide produced by the storm in Jalisco.
A tropical wave emerged off the northwestern coast of Africa on August 22, 2021, and moved westward across the Atlantic Ocean. The wave fractured over the central Atlantic on August 27, with the northern portion developing into Tropical Storm Kate the following day. The southern portion of the wave continued westward, crossing Central America on September 1, at which time the wave fractured again, with a portion of its northern low-level vorticity center splitting off into the Gulf of Mexico and developing into Tropical Storm Mindy. The parent wave continued into the Eastern Pacific on September 2, and produced disorganized convective activity as it progressed to the south of the Pacific Coast of Mexico, leading to the formation of an area of low pressure on September 5. The low gradually developed a well-defined center and organized convection, leading to the formation of Tropical Depression Fifteen-E by 12:00 UTC on September 7. [1]
The depression's inner-core convection was disheveled for a while after formation, but the cyclone organized and became better defined throughout September 8, as it drifted northward within weak steering currents. [1] [2] At 12:00 UTC on the same day, the cyclone strengthened into a tropical storm and was given the name Olaf. [3] Turning northwestward at a slow pace, Olaf developed banding features and good outflow within very favorable environmental conditions for intensification, featuring warm sea-surface temperatures (SSTs) and low amounts of vertical wind shear. [4] On September 9, the storm developed a well-defined eye and rapidly intensified into a Category 1 hurricane around 12:00 UTC. [1] [5] Olaf intensified at an even quicker rate as it neared to southwestern coast of the Baja California Peninsula, developing a symmetrical eyewall as its winds increased by 20 mph in just six hours. [6] At 02:50 UTC on September 10, Olaf reached peak intensity with maximum sustained winds of 105 mph (169 km/h) and a minimum barometric pressure of 968 millibars (28.6 inHg); the storm made landfall very near San José del Cabo at this time. [7] [8]
Olaf's center briefly crossed Baja California Sur before re-emerging back over water, weakening back to Category 1 status in the process. [9] Shortly after emerging back over water, the organization of Olaf collapsed, including its eye and eyewall, and it was downgraded to a tropical storm by 12:00 UTC. [1] [10] Gradually moving westward away from land, Olaf continued to rapidly weaken, with its low-level center becoming exposed and devoid of any deep convection by 21:00 UTC. [11] By 06:00 UTC on September 11, Olaf had been devoid of any organized deep convection for 12 hours, and was therefore designated a remnant low as it turned back to the southwest. [12] The low continued westward for another day before degenerating into a trough of low pressure on September 12. [1]
At 03:00 UTC on September 8, tropical storm watches were issued for southern portions of Baja California Sur. [13] These were extended northward at 09:00 UTC before tropical storm warnings were issued for the same areas. [14] These remained until 09:00 UTC on September 9, when hurricane warnings were issued and tropical storm warnings were extended northward. [15] Hurricane and tropical storm warnings were once again extended northward twelve hours later at 21:00 UTC, six hours before landfall. [16] A red alert was issued statewide. [17] Up to 6 in (150 mm) of rainfall was anticipated for the states of Baja California Sur, Sinaloa, and Nayarit as Olaf approached, along with potential surf of up to 23 ft (7.0 m). [18] Before landfall, ports and schools were closed and residents living in flood zones were urged to evacuate. [19] COVID-19 vaccinations were suspended and 20,000 tourists fled to hotels. [20] 20 temporary shelters were set up in Baja California Sur for residents with homes in high-risk areas of impact. [21] Classes in Cabo San Lucas were suspended on September 10. [22]
The Federal Electricity Commission (CFE) of Mexico reported that over 191,000 people lost electricity at the height of the storm. [21] By September 12, with the help of 678 electrical workers, 110 cranes, 212 vehicles and 2 helicopters, power had been restored to 94% of the affected population. [23] Moisture associated with Olaf resulted in heavy rains and flash flooding across the state of Jalisco, causing the collapse of a trailer near Mexican Federal Highway 80 and an associated fatality. [24] Heavy rains from both Olaf and Hurricane Nora, which affected northwestern Mexico less than two weeks prior, prompted the closure of beaches across the neighboring state of Nayarit. [25] Heavy rain, strong winds, and high waves buffeted the southwest coast of the Baja California Peninsula. [26] [27] Olaf brought powerful winds and heavy rainfall to Baja California Sur. Hotels in the state received minor damage, and some motorists were trapped in their vehicles; numerous fallen trees were also reported. [28] A total of thirty-seven airline flights were cancelled due to the hurricane. [29] Damage across Mexico was estimated at MXN$380 million (USD$19 million), with MXN$200 million (USD$10 million) in damage occurring in the municipalities of Los Cabos and La Paz alone. [30] [31]
The 2003 Pacific hurricane season was the first season to feature no major hurricanes – storms of Category 3 intensity or higher on the Saffir–Simpson hurricane wind scale (SSHWS) – since 1977. The dates conventionally delimiting the period when most tropical cyclones form in the Pacific Ocean are May 15 in the Eastern Pacific Ocean and June 1 in the Central Pacific, with both seasons ending on November 30. The 2003 season featured 16 tropical storms between May 19 and October 26; 7 of these became hurricanes, which was then considered an average season. Damage across the basin reached US$129 million, and 23 people were killed by the storms.
Hurricane Javier was a powerful tropical cyclone whose remnants brought above-average rainfall totals across the western United States in September 2004. Javier was the tenth named storm, the sixth hurricane and the final major hurricane of the 2004 Pacific hurricane season. Javier was also the strongest hurricane of the 2004 season, with 150 mph (240 km/h) winds and a central pressure of 930 millibars. However, because of high wind shear in the East Pacific, Javier weakened rapidly before making landfall in Baja California as a tropical depression. The remnants of the storm then continued moving northeast through the Southwestern United States. Javier caused no direct fatalities, and the damage in Mexico and the United States was minimal.
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.
Hurricane Greg was the only eastern Pacific tropical cyclone in 1999 to make a direct landfall. Part of the annual hurricane season, Greg originated from a tropical wave that departed Africa in mid-August. The wave entered the eastern Pacific by September 1, steadily organizing over subsequent days to become a tropical depression on September 5. Amid a favorable environment, the cyclone intensified into Tropical Storm Greg a few hours after formation and further organized into a Category 1 hurricane on September 6. Greg paralleled the southwestern coastline of Mexico, where it destroyed over 250 homes, cut-off roads, killed 10 people, and left at least 4,000 more injured. The storm weakened to tropical storm intensity as it moved ashore Baja California Sur, although rain was generally beneficial there. Succumbing to cooler waters and high wind shear, Greg ultimately dissipated over the Pacific on September 9. Its remnants led to thunderstorms across northern California, with only minor impacts.
The 2013 Pacific hurricane season was the first to see twenty named storms since 2009 but also had the ninth fewest ACE units on record, as many of the storms were weak and short-lived. The season officially began on May 15 in the Eastern Pacific and started on June 1 in the Central Pacific; both ended on November 30. These dates conventionally delimit the period of each year when most tropical cyclones form east of the International Dateline in the North Pacific basin. The first cyclone, Tropical Storm Alvin, formed on May 15, and the last, Tropical Storm Sonia, dissipated on November 4.
The 2017 Pacific hurricane season was an above average Pacific hurricane season in terms of named storms, though less active than the previous three, featuring eighteen named storms, nine hurricanes, and four major hurricanes. Despite the considerable amount of activity, most of the storms were weak and short-lived. The season officially started on May 15 in the eastern Pacific Ocean, and on June 1 in the central Pacific; they both ended on November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the respective regions. However, the formation of tropical cyclones is possible at any time of the year, as illustrated in 2017 by the formation of the season's first named storm, Tropical Storm Adrian, on May 9. At the time, this was the earliest formation of a tropical storm on record in the eastern Pacific basin proper. The season saw near-average activity in terms of accumulated cyclone energy (ACE), in stark contrast to the extremely active seasons in 2014, 2015, and 2016; and for the first time since 2012, no tropical cyclones formed in the Central Pacific basin. However, for the third year in a row, the season featured above-average activity in July, with the ACE value being the fifth highest for the month. Damage across the basin reached $375.28 million (2017 USD), while 45 people were killed by the various storms.
The 2013 Pacific hurricane season was an above-average year in which twenty named storms developed. The hurricane season officially began on May 15 in the East Pacific, coinciding with the formation of Tropical Storm Alvin, and on June 1 in the Central Pacific; it ended on November 30 in both basins. These dates conventionally delimit the period during each year when most tropical cyclones form. The final system of the year, Tropical Storm Sonia, dissipated on November 4.
Hurricane Blanca in 2015 was the earliest recorded tropical cyclone in the calendar year to make landfall on the Baja California Peninsula. Forming as a tropical depression on May 31, Blanca initially struggled to organize due to strong wind shear. However, once this abated, the system took advantage of high sea surface temperatures and ample moisture. After becoming a tropical storm on June 1, Blanca rapidly intensified on June 2–3, becoming a powerful Category 4 hurricane on the Saffir–Simpson hurricane wind scale; maximum sustained winds reached 145 mph (230 km/h) at this time. The hurricane's slow motion resulted in tremendous upwelling of cooler water, resulting in a period of weakening. Blanca gradually recovered from this and briefly regained Category 4 status on June 6 as it moved generally northwest toward the Baja California peninsula. Cooler waters and increased shear again prompted weakening on June 7 and the system struck Baja California Sur on June 8 as a weak tropical storm. It quickly degraded to a depression and dissipated early the next day.
Hurricane Sandra was the latest-forming major hurricane in the northeastern Pacific basin, the strongest Pacific hurricane on record in November, and the record eleventh major hurricane of the 2015 Pacific hurricane season. Originating from a tropical wave, Sandra was first classified as a tropical depression on November 23 well south of Mexico. Environmental conditions, including high sea surface temperatures and low wind shear, were highly conducive to intensification and the storm quickly organized. A small central dense overcast developed atop the storm and Sandra reached hurricane status early on November 25 after the consolidation of an eye. Sandra reached its peak intensity as a Category 4 hurricane on the Saffir–Simpson hurricane wind scale with winds of 150 mph (240 km/h) and a pressure of 934 mbar early on November 26. Thereafter, increasing shear degraded the hurricane's structure and weakening ensued. Rapid weakening took place on November 27 and Sandra's circulation became devoid of convection as it diminished to a tropical storm that evening. The cyclone degenerated into a remnant low soon thereafter and ultimately dissipated just off the coast of Sinaloa, Mexico, on November 29.
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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The 2022 Pacific hurricane season was an active hurricane season in the eastern North Pacific basin, with nineteen named storms, ten hurricanes, and four major hurricanes. Two of the storms crossed into the basin from the Atlantic. In the central North Pacific basin, no tropical cyclones formed. The season officially began on May 15 in the eastern Pacific, and on June 1 in the central; both ended on November 30. These dates historically describe the period each year when most tropical cyclogenesis occurs in these regions of the Pacific and are adopted by convention.
Tropical Storm Narda was a short-lived tropical storm that remained close to the Pacific coast of Mexico, causing flash flooding and mudslides in southwestern Mexico and the Baja California Peninsula in late September 2019. The fourteenth named storm of the 2019 Pacific hurricane season, Narda developed from a broad area of low pressure that formed off the Central American Pacific coast on September 26. The broad low gradually organized as it moved west-northwestward, and it became Tropical Storm Narda early on September 29 while located off the southern coast of Mexico. The cyclone strengthened slightly before it moved inland near Manzanillo. Narda weakened to a tropical depression after moving inland, but restrengthened into a tropical storm on September 30 as it emerged over the Pacific Ocean just south of the Gulf of California. Narda quickly strengthened, and reached its peak intensity with winds of 50 mph (85 km/h) that day before making a second landfall along the northwestern coast of Mexico. The tropical cyclone weakened rapidly as it moved along the coastline, and it weakened to a tropical depression before dissipating just off the coast of Sonora on October 1.
Hurricane Genevieve was a strong tropical cyclone that almost made landfall on the Baja California Peninsula in August 2020. Genevieve was the twelfth tropical cyclone, eighth named storm, third hurricane, and second major hurricane of the 2020 Pacific hurricane season. The cyclone formed from a tropical wave that the National Hurricane Center (NHC) first started monitoring on August 10. The wave merged with a trough of low pressure on August 13, and favorable conditions allowed the wave to intensify into Tropical Depression Twelve-E at 15:00 UTC. Just six hours later, the depression became a tropical storm and was given the name Genevieve. Genevieve quickly became a hurricane by August 17, and Genevieve began explosive intensification the next day. By 12:00 UTC on August 18, Genevieve reached its peak intensity as a Category 4 hurricane, with maximum 1-minute sustained winds of 130 mph and a minimum central pressure of 950 millibars (28 inHg). Genevieve began to weaken on the next day, possibly due to cooler waters caused by Hurricane Elida earlier that month. Genevieve weakened below tropical storm status around 18:00 UTC on August 20, as it passed close to Baja California Sur. Soon afterward, Genevieve began to lose its deep convection and became a post-tropical cyclone by 21:00 UTC on August 21, eventually dissipating off the coast of Southern California late on August 24.
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Hurricane Nora was a large tropical cyclone that caused significant damage across the Pacific Coast of Mexico in late August 2021. The fourteenth named storm and fifth hurricane of the 2021 Pacific hurricane season, Nora was first monitored by the National Hurricane Center (NHC) as an area of low pressure near the coast of Mexico. On August 24, the low organized into tropical depression, but struggled to develop further due to wind shear in its surrounding environment. The depression eventually intensified into a tropical storm and was named Nora as it tracked to the west-northwest. Nora peaked as a strong Category 1 hurricane with maximum sustained winds of 85 miles per hour (140 km/h) on August 28. The storm then grazed the west coast of Mexico and made landfall two separate times, first in the state of Jalisco, followed by neighboring Nayarit. Nora weakened as it interacted with land, dissipating on August 30 just inland of the Mexican coast.
This article incorporates public domain material from websites or documents of the National Weather Service .