Meteorological history | |
---|---|
Formed | September 1,1998 |
Remnant low | September 3,1998 |
Dissipated | September 8,1998 |
Category 1 hurricane | |
1-minute sustained (SSHWS/NWS) | |
Highest winds | 75 mph (120 km/h) |
Lowest pressure | 988 mbar (hPa);29.18 inHg |
Overall effects | |
Fatalities | 14 |
Damage | $100 million |
Areas affected | Baja California Peninsula,Northern Pacific coast of Mexico,Southwestern United States,Northwestern United States |
IBTrACS | |
Part of the 1998 Pacific hurricane season |
Hurricane Isis was the only hurricane to make landfall during the 1998 Pacific hurricane season. The ninth tropical storm and sixth hurricane of the season,Isis developed on September 1 from an interaction between a tropical wave and a large surface circulation to the southwest of Mexico. It moved northward,striking the extreme southeastern portion of the Baja California peninsula before attaining hurricane status in the Gulf of California. Isis made landfall at Topolobampo in the Mexican state of Sinaloa on September 3,and quickly lost its low-level circulation. The remnants persisted for several days before dissipating over the U.S. state of Idaho on September 8.
In Mexico,Isis destroyed over 700 houses and killed 14 people;this is primarily due to its heavy rainfall which peaked at over 20 inches (510 mm) in southern Baja California Sur. The rainfall caused widespread damage to roads and railways,stranding thousands of people. Moisture from the remnants of Isis extended into the southwestern United States,resulting in light rainfall,dozens of traffic accidents,and power outages to thousands of residents in San Diego County,California.
A tropical wave moved off the coast of Africa on August 14, 1998. It traveled westward, and on August 19 spawned the tropical depression that eventually became Hurricane Bonnie. [1] The wave continued westward across the Atlantic Ocean and Caribbean Sea, and crossed Central America into the eastern Pacific Ocean on August 25. The wave decreased its forward speed while approaching a large low-level circulation over southern Mexico. A broad area of disturbed weather formed in association with the wave and the low-level circulation, and after persisting for several days developed a smaller low-level circulation on August 29 about 575 miles (925 km) south-southeast of Cabo San Lucas. On August 31, the two primary areas of convection were well-removed from the center. By early on September 1, despite a lack of convective organization, the low-cloud circulation was sufficiently well-defined that the National Hurricane Center designated it as Tropical Depression Ten-E, or the tenth tropical depression of the season, about 350 miles (560 km) south of Cabo San Lucas. [2] In real time, the National Hurricane Center first upgraded the system 21 hours later. [3]
The depression initially tracked slowly north-northwestward and gradually strengthened. Late on September 1 it intensified into Tropical Storm Isis while located about 200 miles (320 km) south of Cabo San Lucas. [2] Upon becoming a tropical storm, the deep convection was not organized, causing one forecaster to describe Isis as a large monsoon-like system. [3] A mid-level trough extending southward from the Arizona/California border caused the storm to accelerate northward. The storm quickly strengthened; six hours after Isis became a tropical storm it reached winds of 70 mph (110 km/h). [2] Very deep, symmetrical convection developed over the poorly defined center of circulation while banding features began to form, although ill-defined outflow and land interaction with the Baja California Peninsula initially prevented further strengthening. [4] At 1200 UTC on September 2, Isis made landfall on extreme southeastern Baja California Sur as a strong tropical storm, and subsequently turned to the north-northeast. [2]
After entering the Gulf of California, an eye began to become apparent on visible satellite imagery, and it is estimated Isis attained hurricane status late on September 2. Continuing northward, it struck Topolobampo in the state of Sinaloa early on September 3 as a minimal hurricane. Isis weakened to a tropical storm a few hours after landfall, and subsequent to turning to the north-northwest the low-level circulation dissipated over Sierra Madre Occidental. [2] The remnants entered southern Arizona on September 4 and tracked around an upper-level low. After entering Nevada on September 5, the remnants of Isis passed into Oregon, before dissipating over Idaho on September 8. [5]
Coinciding with the National Hurricane Center's first advisory on Isis, the government of Mexico issued a tropical storm warning from Dolores to Puerto Cortés along the Baja California Peninsula. This helped some of the residents get an early start. Early on September 2, the warning was extended from Santa Rosalía to Punta Abreojos, while an additional tropical storm warning was issued from El Dorado to Guaymas. After Isis became a hurricane, officials issued a hurricane warning from Dolores to Punta San Gabriel on the Baja California Peninsula and from El Dorado to Bahía Kino on the mainland. [2]
In Baja California Sur, 2,500 residents were evacuated to emergency shelters. Officials closed the port at Mazatlán and recommended fisherman along the coast of the Gulf of California to remain at port. [6] Officials set up 49 shelters on the mainland to provide evacuees with food, clothing and medical attention. [7] The Mexican Army assisted residents in evacuation, and the Navy provided medical aid and assistance to boat owners. More than 24,000 people were sheltered during the storm. [8]
Isis first affected Baja California Sur on September 2 as a tropical storm. Shortly after making landfall, a weather reporting station at San José del Cabo recorded sustained winds of 26 mph (42 km/h), and gusts reaching up to 46 mph (74 km/h). A station on the Islas Marías also reported sustained winds of 54 mph (87 km/h). [2] The winds left widespread areas without power or telephone. [6] The storm produced heavy rainfall in the southern portion of the peninsula, including a 24‑hour total of 12.99 inches (330 mm) at Los Cabos [2] and a peak rainfall total of 24.02 inches (610 mm) at Santiago. [5] A married couple was killed after attempting to cross a flooded stream in Los Cabos. [6] [9] Initially, reports indicated a family was missing in La Paz, though they were later proven false. [6] Flooding from the storm closed all roads to the north of Los Cabos and caused damage to the roads in the area. Mudslides from the rain buried at least 120 cars in the area. [9]
Rainfall reached over 10 inches (250 mm) in the coastal region of Jalisco, and lighter amounts of precipitation extended further to the southeast and northeast. [5] One person was reported missing in Jalisco. [7] The heaviest 24‑hour rainfall total in the state of Sinaloa was 8.66 inches (220 mm), whereas in Sonora a maximum of 4.72 inches (120 mm) of rain were recorded. [2] Strong waves from the hurricane struck the Mexican mainland, with four people injured at Mazatlán when their boat washed onto rocks and was destroyed. [6] Rainfall from the storm flooded 15 communities in and around Mazatlán, and the Army assisted residents in emergency evacuations. [7] At Los Mochis, near the point where Isis made landfall, the hurricane resulted in the destruction of 300 homes, as well as in seven fatalities. [10] Throughout the city, strong winds from the hurricane downed street posts, tree limbs, and power lines, with one person seriously injured from a downed power line. Additionally, the roof of a gas station collapsed from the winds. [7] More than 1,200 bus passengers in Sinaloa were stranded due to road closures from the hurricane, [10] including the closure of the coastal highway in the southern portion of Sinaloa as it had been washed out due to floodwaters. Rainfall from the storm caused severe river flooding in some locations, and authorities advised those living along the Fuerte River to be prepared for a possible evacuation. [11] The winds from Isis left about 120,000 people in the municipality of Ahome without power. [8]
Throughout Mexico, the passage of Hurricane Isis resulted in 14 deaths and the loss of 769 homes, [2] with property damage estimates totaling over $5 million (1998 USD, 50 million 1998 MXN, $6.3 million 2007 USD). [12] According to a speech by President Ernesto Zedillo, Isis damaged the water systems in 173 localities; it also damaged 154 primary schools and nine high schools, minor in most cases, causing most schools to be closed for around a week. A total of 730 miles (1,170 km) of railroad track was damaged by mudslides or flooding, with one bridge entirely destroyed and another four damaged. [8]
Thunderstorms from the remnants of Isis dropped more than two inches (51 mm) of rainfall across southern Arizona, resulting in some flash flood warnings and flooding on roadways. [13] The heaviest precipitation fell across the Santa Catalina and Rincon Mountains near Tucson, which saw precipitation amounts of up to three inches (76 mm). Otherwise, no flooding was reported in the Tucson area, and the Tucson International Airport reported only 1.1 inches (28 mm) as a result of the storm. [14]
The moisture extended into southern California and produced moderate precipitation across the region. Bakersfield reported a one-day rainfall record on September 4 with 0.23 inches (5.8 mm) of precipitation, breaking the previous record of 0.17 inches (4.3 mm) set in 1963. Rainfall amounts at Frazier Park peaked at 1.53 inches (39 mm). Agricultural losses, primarily from vintners and raisin growers, rose up to $5 million in damage (1998 USD, $6.33 million 2007 USD), either directly due to rain or indirectly due to the additional steps to treat the increase in fungus activity on produce. [15] Slick roads from the rain resulted in nearly 80 traffic accidents in San Diego County, ranging from fender benders to moderate injuries. Thunderstorms from the remnants of Isis damaged a San Diego Gas & Electric substation at Kearny Mesa, leaving 10,000 customers without power; the outage was short lived and completely restored within two hours. About 1,000 homes and businesses were temporarily without power in Escondido, and another 2,700 customers lost electricity in Rancho Bernardo. Rainfall in and around San Diego reached a maximum of 0.5 inches (13 mm) at La Mesa. [16] Heavy clouds from Isis produced scattered rainfall and temporary relief to severe heat conditions in the Los Angeles area. [17]
Moisture from the remnants of Isis spread across the southwestern United States, and rainfall reached over 0.75 inches (19 mm) in Nevada and Utah. Low-level moisture dissipated as it continued inland, due to dry air, although upper-level moisture produced light rain across the Northwestern United States; Pocatello, Idaho recorded 0.59 inches (15 mm), while Missoula, Montana recorded 0.39 inches (9.9 mm). [18]
Aid programs began immediately after Isis moved ashore and dissipated to provide support to the affected population. The Comisión Nacional del Agua distributed 1.6 million U.S. gallons (1.3 million imp gal/6 million L) of water and provided repair equipment to the 173 localities whose water systems were damaged. More than 650 health workers worked to combat the spread of diseases, including monitoring sanitary conditions of water and foods, and sprayed nearly 9,900 acres (40 km2) of land to prevent the breeding of mosquitoes. The force also disinfected more than 6,600 latrines and removed more than 850 short tons (770 t ) of sewage to prevent the spread of epidemic. No medical-related deaths occurred as a result of this attention. [8]
Twenty-four hours after the passage of the hurricane, workers had restored power to 70% of the affected residents in Sinaloa, and by six days after the storm, electrical service was completely restored. The damage to the federal highway between Culiacán and Los Mochis along the coastal region of Sinaloa was restored about 48 hours after the passage of the hurricane. The rehabilitation of the agricultural infrastructure began immediately, and most of the drainage networks were repaired by about two weeks after the hurricane. About half of the damaged railways were repaired by about a month after the storm. The total cost for reconstruction and aid amounted to about $18.5 million (1998 USD, 175 million 1998 MXN$, 34.6 million in 2024 USD), about 94% from federal funds and the rest from state funding. A portion of the funding was allocated to assist the reconstruction of destroyed houses. [8]
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.
Hurricane Ismael was a weak, but deadly Pacific hurricane that killed over one hundred people in northern Mexico in September of the 1995 Pacific hurricane season. It developed from a persistent area of deep convection on September 12, and steadily strengthened as it moved to the north-northwest. Ismael attained hurricane status on September 14 while located 210 miles (340 km) off the coast of Mexico. It continued to the north, and after passing a short distance east of Baja California Sur it made landfall on Topolobampo in the state of Sinaloa with winds of 80 mph (130 km/h). Ismael rapidly weakened over land, and dissipated on September 16 over northwestern Mexico. The remnants entered the United States and extended eastward into the Mid-Atlantic States.
Hurricane Marty was a Category 2 Pacific hurricane that caused extensive flooding and damage in northwestern Mexico just weeks after Hurricane Ignacio took a similar course. Marty was the thirteenth named storm, fourth hurricane, and the deadliest tropical cyclone of the 2003 Pacific hurricane season. Forming on September 18, it became the 13th tropical storm and fourth hurricane of the year. The storm moved generally northwestward and steadily intensified despite only a marginally favorable environment for development, and became a Category 2 hurricane before making two landfalls on the Baja California peninsula and mainland Mexico.
Hurricane John was a Category 4 hurricane that caused heavy flooding and extensive damage across most of the Pacific coast of Mexico in late August through early September 2006. John was the eleventh named storm, seventh hurricane, and fifth major hurricane of the 2006 Pacific hurricane season. Hurricane John developed on August 28 from a tropical wave to the south of Mexico. Favorable conditions allowed the storm to intensify quickly, and it attained peak winds of 130 mph (210 km/h) on August 30. Eyewall replacement cycles and land interaction with western Mexico weakened the hurricane, and John made landfall on southeastern Baja California Sur with winds of 110 mph (180 km/h) on September 1. It slowly weakened as it moved northwestward through the Baja California peninsula, and dissipated on September 4. Moisture from the remnants of the storm entered the southwest United States.
Hurricane Paul was a Category 2 Pacific hurricane that struck Mexico as a tropical depression in October 2006. The seventeenth named storm and tenth hurricane of the annual hurricane season, Paul developed from an area of disturbed weather on October 21. The cyclone slowly intensified as it moved into an area of warm waters and progressively decreasing wind shear. Paul attained hurricane status on October 23, and later that day the storm reached its peak intensity with maximum sustained winds of 105 mph (169 km/h), a strong Category 2 hurricane on the Saffir-Simpson scale. A strong trough turned the hurricane to the north and northeast into an area of strong vertical shear, and Paul weakened to a tropical storm on October 24. It accelerated northeastward, and after passing a short distance south of Baja California Sur the low level circulation became decoupled from the rest of the convection. Paul weakened to a tropical depression on October 25 a short distance off the coast of Mexico, and after briefly turning away from the coast it made landfall on northwestern Sinaloa on October 26. The depression dissipated shortly thereafter.
Hurricane Ignacio was the latest-forming first hurricane of a Pacific hurricane season since reliable satellite observation began in 1966. The ninth tropical storm of the 2003 Pacific hurricane season, Ignacio developed out of a tropical wave on August 22 a short distance off the coast of Mexico. It was initially predicted to track out to sea and remain a weak tropical storm, though it unexpectedly organized rapidly to attain peak winds of 105 mph (169 km/h) on August 24 while located a short distance southeast of southern Baja California Sur. Land interaction weakened Ignacio to an 80 mph (130 km/h) hurricane by the time it made landfall near La Paz, and it dissipated on August 27 in the central Baja California peninsula.
Hurricane Lester was the first Pacific tropical cyclone to enter the United States as a tropical storm since 1967. The fourteenth named storm and eighth hurricane of the 1992 Pacific hurricane season, Lester formed on August 20 from a tropical wave southwest of Mexico. The tropical storm moved generally northwestward while steadily intensifying. After turning to the north, approaching the Mexican coast, Lester attained hurricane status. The hurricane reached peak winds of 85 mph (137 km/h) before making landfall on west-central Baja California. The system weakened while moving across the peninsula and then over northwestern Mexico. Not long after entering Arizona, Lester weakened to a tropical depression, and degenerated into an extratropical low on August 24, 1992, over New Mexico. The storm's remnants later merged with the remnants of Hurricane Andrew and another frontal system on August 29.
Hurricane Madeline was a costly tropical cyclone whose remnants caused hundreds of millions of dollars in damage in Texas in October 1998. The final tropical cyclone of the 1998 Pacific hurricane season, Madeline originated from a tropical wave that emerged off the coast of Africa on September 25, 1998. The wave traversed the Atlantic Ocean and crossed over Central America on October 5 or 6. Gradually, the system intensified and was classified as a tropical depression on October 16, a tropical storm later that day, and a hurricane on October 17. The storm reached peak winds of 85 mph (137 km/h) about 95 miles (153 km) southwest of San Blas, Nayarit, and after 18 hours it subsequently began to weaken. Although Madeline never made landfall, numerous rainbands affected the Mexican coast causing no known damage or fatalities. The remnant moisture moved north and contributed to flooding in central Texas, which killed 31 people and caused $750 million in damage.
Hurricane Fausto was a Pacific hurricane that caused light damage to Baja California Sur in September 1996. On September 10, a tropical depression developed a short distance south-southeast of the Mexican Riviera. Slowly intensifying, Fuasto paralleled the coastline. It became a hurricane on September 12, and after briefly reaching major hurricane intensity, increasing wind shear resulted in a weakening trend. It traversed Baja California Sur on September 13 as minimal hurricane, and struck Sinaloa the next day. Inland, it degenerated into a remnant circulation by September 15. Fausto's remnants continued moving eastward across the Gulf of Mexico and later emerged into the Atlantic, before developing into a large nor'easter on September 17. Afterward, the system moved northeastward, before it was last noted on September 18.
Tropical Storm Julio was a tropical storm that made landfall on the southern tip of Baja California Sur in August 2008. The eleventh named storm of the 2008 Pacific hurricane season, it developed from a tropical wave on August 23 off the coast of Mexico. It moved parallel to the coast, reaching peak winds of 50 mph (85 km/h) before moving ashore and weakening. On August 26 it dissipated in the Gulf of California. Julio was the third tropical cyclone to make landfall in the Eastern Pacific tropical cyclone basin during the season, after Tropical Storm Alma, which struck Nicaragua in May, and Tropical Depression Five-E, which moved ashore along southwestern Mexico in July. The storm brought locally heavy rainfall to southern Baja California, killing one person and leaving several towns isolated. Moisture from Julio reached Arizona, producing thunderstorms, including one which damaged ten small planes in Chandler.
Hurricane Rosa was the only Pacific hurricane to make landfall during the above-average 1994 Pacific hurricane season. It killed at least 4 people in Mexico. Moisture from the hurricane was a factor in widespread flooding in the U.S. state of Texas that killed 22 people and caused hundreds of millions of dollars in damage in October 1994. The pre-Rosa tropical depression formed on October 8 before degenerating the next day. It reformed on October 10 and steadily strengthened as it approached Mexico. Ultimately peaking as a Category 2 hurricane on the Saffir-Simpson Hurricane Scale right before landfall, Rosa was the final hurricane, nineteenth tropical storm, and second-last tropical cyclone of the 1994 Pacific hurricane season.
Hurricane Norbert is tied with Hurricane Jimena as the strongest tropical cyclone to strike the west coast of Baja California Sur in recorded history. The fifteenth named storm, seventh hurricane, and second major hurricane of the 2008 hurricane season, Norbert originated as a tropical depression from a tropical wave south of Acapulco on October 3. Strong wind shear initially prevented much development, but the cyclone encountered a more favorable environment as it moved westward. On October 5, the National Hurricane Center (NHC) upgraded the depression to Tropical Storm Norbert, and the system intensified further to attain hurricane intensity by October 6. After undergoing a period of rapid deepening, Norbert reached its peak intensity as a Category 4 on the Saffir–Simpson hurricane wind scale, with maximum sustained winds of 135 mph (217 km/h) and a minimum barometric pressure of 945 mbar. As the cyclone rounded the western periphery of a subtropical ridge over Mexico, it began an eyewall replacement cycle which led to steady weakening. Completing this cycle and briefly reintensifying into a major hurricane, a Category 3 or higher on the Saffir–Simpson hurricane wind scale, Norbert moved ashore Baja California Sur as a Category 2 hurricane late on October 11. After a second landfall at a weaker intensity the following day, the system quickly weakened over land and dissipated that afternoon.
Tropical Storm Lowell was a moderate tropical storm that developed during the 2008 Pacific hurricane season. The fourteenth tropical cyclone and thirteen named storm of the season, Lowell formed out of a western side of a trough on September 6. It quickly intensified into Tropical Storm Lowell, peaking as a moderate tropical storm. It pass directly over Socorro Island and began a weakening trend. It weakened into depression before landfall in Baja California Sur and dissipated before striking Sonora. It later joined with a frontal boundary and Hurricane Ike which caused severe damage as far inland as Chicago. In all, the storm had caused 6 deaths and $15.5 million damage.
Hurricane Paine was the sixteenth tropical storm and eighth hurricane of the fairly active 1986 Pacific hurricane season; moisture from the system contributed to one of the most significant flooding events in Oklahoma history. Paine formed on September 28 off the southeast coast of Mexico. It moved around a ridge, later turning to the north and brushing the Baja California Peninsula. By that time, Paine had attained peak winds of 100 mph (160 km/h), but it weakened slightly before hitting the Mexican state of Sonora. The remnant moisture combined with a cold front to produce heavy rainfall in the South Central United States.
Hurricane Bud was a tropical cyclone that brought winds and severe flooding to Mexico throughout its existence as a tropical cyclone in June 2018. It was the second named storm, hurricane, and major hurricane of the 2018 Pacific hurricane season. Bud originated from a tropical wave that departed from Western Africa on May 29. It traveled across the Atlantic Ocean before entering the Northeast Pacific Ocean late on June 6. The system moved towards the northwest and steadily organized, becoming a tropical depression on June 9 and Tropical Storm Bud early the next day. Favorable upper-level winds, ample moisture aloft, and warm sea surface temperatures allowed the storm to rapidly intensify to a hurricane late on June 10, and further to a major hurricane on the following day. Bud ultimately peaked the next morning with maximum sustained winds of 140 mph (230 km/h) and a minimum central pressure of 943 mbar. Its track curved more northward while the storm rapidly succumbed to the effects of upwelling. Bud made landfall on Baja California Sur as a minimal tropical storm early on June 15. On the next day, land interaction and increasing wind shear caused Bud to degenerate into a post-tropical cyclone. It opened up into a trough of low-pressure on June 16. The remnants of Bud moved towards the Southwestern United States, bringing tropical moisture and gusty winds to the region.
Tropical Depression Nineteen-E was a weak yet costly tropical cyclone that caused significant flooding throughout Northwestern Mexico and several states within the United States in September 2018. The storm was also the first known tropical cyclone to form over the Gulf of California. Nineteen-E originated from a tropical wave that left the west coast of Africa on August 29 to 30. It continued westward, crossed over Central America, and entered the northeastern Pacific Ocean by September 7. It then meandered to the southwest of Mexico for the next several days as it interacted with a mid-to-upper level trough. The National Hurricane Center (NHC) continued to track the disturbance for the next several days as it traveled northward. A surface trough developed over the Baja California peninsula on September 18. Despite disorganization and having close proximity to land, the disturbance developed into a tropical depression in the Gulf of California on September 19, after having developed a circulation center and more concentrated convection. The system peaked with maximum sustained winds of 35 mph (55 km/h) and a minimum central pressure of 1002 mbar.
Hurricane Norma was one of four tropical cyclones to strike the Pacific Coast of Mexico in October 2023. The seventeenth tropical depression, fourteenth named storm, ninth hurricane and seventh major hurricane of the 2023 Pacific hurricane season, Norma developed from an area of low pressure that formed off the coast of southern Mexico on October 15, 2023. The disturbance gradually organized as it progressed westward parallel to the coast, and developed into Tropical Storm Norma on October 17. Turning northward, Norma rapidly intensified to a Category 4 hurricane as it continued to parallel the west coast of Mexico. Less favorable environmental conditions caused Norma to gradually weaken as it approached the Baja California peninsula. The cyclone made landfall on the Mexican state of Baja California Sur as a Category 1 hurricane. Norma continued to weaken as it crossed the state. The storm emerged over the Gulf of California on October 22, and made landfall as a tropical depression the following day on the state of Sinaloa. Norma quickly dissipated as it moved inland over Mexico.