Tropical Storm Lowell (2008)

Last updated
Map key
  Tropical depression (≤38 mph, ≤62 km/h)
  Tropical storm (39–73 mph, 63–118 km/h)
  Category 1 (74–95 mph, 119–153 km/h)
  Category 2 (96–110 mph, 154–177 km/h)
  Category 3 (111–129 mph, 178–208 km/h)
  Category 4 (130–156 mph, 209–251 km/h)
  Category 5 (≥157 mph, ≥252 km/h)
  Unknown
Storm type
Disc Plain black.svg Tropical cyclone
Solid black.svg Subtropical cyclone
ArrowUp.svg Extratropical cyclone, remnant low, tropical disturbance, or monsoon depression

The origin of Lowell began from a tropical wave that moved off Africa. The northern portion of the wave would form into Hurricane Hanna in the Atlantic. The southern portion of the wave separated and continued to move westward across the Caribbean and crossed Central America during August 27 and August 28. [1] Later a trough with a weak low pressure area developed over southern Mexico, The area of low pressure was found embedded within a large area of scattered moderate and isolated strong convection. [2] The initial low failed to develop [3] but a new low formed on western side of the trough. A larger cyclonic circulation associated with the trough and induced a gradual increase in deep convection. [4] The low level convection center was temporarily displaced from the convection, and a smaller embedded circulation developed and was eventually detached from the larger circulation. It is estimated that a tropical depression formed at 1200 UTC 6 September when it was centered about 310 mi (500 km) south of Manzanillo, Mexico. [5]

As convective banding formed, the depression gradually intensified and was upgraded a Tropical Storm Lowell six hours later. [6] A deep-layer anticyclone over Mexico steered Lowell northwestward until September 8. However, strong upper-level winds on the south side of the anticyclone produced strong northeasterly to easterly wind shear over the tropical cyclone for several days. Due to the shear, the low level convection became exposed and sheared. despite this, Lowell slowly strengthened and reached a peak intensity of 50 mph (85 km/h), it then passed near Socorro Island without any known damage. The shear had lessened over the system, but with stable and dry air, the storm begin to weaken. [7] Lowell moved towards north and northeast due to a subtropical ridge northwest of the system. It downgraded to a tropical depression at 0600 UTC 10 September as it was moving north-northeastward about 259 mi (417 km) west-southwest of the southern tip of Baja California. [8] Thunderstorm activity near the center had increased slightly on 10 September. The circulation began to slowly spin down as it made landfall around Cabo San Lucas, Mexico at 0900 UTC 11 September. [9] As it made landfall the mid to upper level winds left the low level center exposed form the thunderstorm activity. Lowell degenerated into an elongated surface trough that extended across the southern Gulf of California. [10] It followed a squall line and a frontal boundary and quickly dissipated. The remnant low produced rain across Northwestern Mexico, it later joined Hurricane Ike and caused damage further inland. [1]

Preparations and Impact

Mexico

Tropical Storm Lowell nearing Baja California Peninsula on September 10 Tropical Storm Lowell 2008-09-10.jpg
Tropical Storm Lowell nearing Baja California Peninsula on September 10

On September 9, 2100 UTC a Tropical Storm Watch was issued from Bahia Magdalena to Cabo San Lucas and ended on September 11 0900 UTC. [1] Heavy rainfall from the remnants of Lowell caused streams and canals to overflow in the Mexican states of Sonora and Sinaloa, leaving more than 26,500 people homeless. The cities of Navojoa, Benito Juárez, Huatabampo, and Etchojoa were most affected. The government of Sonora has estimated the damage in that state at 200 million pesos (about 15.5 million US dollars). [1] In its impact route to Baja California Sur, Tropical Storm Lowell causing heavy rains and strong waves, forcing the closure of the port of Cabo San Lucas and the suspension of at least two cruises from Los Angeles, California with more than 2 thousand passengers each. Impact in Baja California Sur, Tropical Storm Lowell causing heavy rains and strong waves, forcing the closure of the port of Cabo San Lucas and the suspension of at least two cruises from Los Angeles, California, with more than 2 thousand passengers each. In its advance, the weather with winds up to 95 kilometers per hour, wreaking havoc on the coast of the Pacific, from Sonora to Nayarit, where they established the green alert (phase approach) by the heavy rains and storm surges. The director of civil protection in Baja California Sur, Jose Gajón of the Toba, said that Lowell has a radius of 800 km so that the whole body is on alert green.

Classes were suspended in Sinaloa, bad weather caused by the weather associated with a low pressure system, caused the closure of boating in the bay Altata and the port of Topolobampo. Flood victims evacuated. The Secretary of Administration and Finance, Óscar Lara, said that permits were granted exemption from payment of toll motorway Culiacán-Las Brisas for vehicles, by flooding in the villages of the municipality of Navolato. In the city of Los Mochis, the mayor, Esteban Valenzuela, said the rain caused the suspension of classes in schools. In Nayarit, the excess water in the marshes and estuaries affect fishermen suffer low catches of shrimp. The State Civil Protection Unit in Sonora blue alert issued for 16 municipalities of the entity and the green alert for 13 locations in the south to the vicinity of Lowell. Recount Damage In Chihuahua, the rains over the past 15 days left six people dead, more than a thousand communities, 15 thousand hectares of crops flooded, 50 solitary and 43 other villages without drinking water. The secretary of Public Security, Javier Cardona Torres, said that after the declaration of emergency Parral and Valle de Allende, these municipalities will help the Natural Disaster Fund. Also released this instance support for municipalities Aldama Coyame, Ojinaga, San Francisco de Conchos, Camargo, La Cruz and Julimes. In Durango and Coahuila, after the opening of the floodgates of dams Lázaro Cárdenas and Francisco Zarco, Civil Protection authorities evacuated thousands of residents in the communities of Abasolo and Rodeo in Durango, while the Comarca Lagunera, Coahuila, was working in strengthening of the river Nazas board. [11]

United States

The remnants of Lowell later merged with a frontal boundary over the central United States and caused heavy rainfall and flooding one to two days before the remnants of Hurricane Ike passed through the region. Heavy rainfall, including multiple 24-hour records, occurred from West Texas northeast to Kansas and northern Illinois and Indiana. Wichita, Kansas, measured a daily record 10.31 inches of rain on 12 September and broke the 24-hour rainfall record of 7.99 inches that had been held since 1911. Lubbock, Texas, measured a 24-hour record rainfall of 7.80 inches which broke the previous record of 5.83 inches set in October 1983. Chicago, Illinois, reported 6.64 inches at O’Hare International Airport, the highest one-day total since records began in 1871. This amount broke the previous daily record of 6.49 inches set in 1987. Numerous people were rescued from stranded vehicles as rainfall flooded city streets. [1]

See also

Related Research Articles

<span class="mw-page-title-main">2003 Pacific hurricane season</span> Hurricane season in the Pacific Ocean

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.

<span class="mw-page-title-main">2000 Pacific hurricane season</span> Hurricane season in the Pacific Ocean

The 2000 Pacific hurricane season was an above-average Pacific hurricane season, although most of the storms were weak and short-lived. There were few notable storms this year. Tropical storms Miriam, Norman, and Rosa all made landfall in Mexico with minimal impact. Hurricane Daniel briefly threatened the U.S. state of Hawaii while weakening. Hurricane Carlotta was the strongest storm of the year and the second-strongest June hurricane in recorded history. Carlotta killed 18 people when it sank a freighter. Overall, the season was significantly more active than the previous season, with 19 tropical storms. In addition, six hurricanes developed. Furthermore, there were total of two major hurricanes.

<span class="mw-page-title-main">1998 Pacific hurricane season</span> Hurricane season in the Pacific Ocean

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.

<span class="mw-page-title-main">2007 Pacific hurricane season</span> Hurricane season in the Pacific Ocean

The 2007 Pacific hurricane season was a below-average Pacific hurricane season, featuring one major hurricane. 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 the region. The first tropical cyclone of the season, Alvin, developed on May 27, while the final system of the year, Kiko, dissipated on October 23. Due to unusually strong wind shear, activity fell short of the long-term average, with a total of 11 named storms, 4 hurricanes, and 1 major hurricane. At the time, 2007 featured the second-lowest value of the Accumulated cyclone energy (ACE) index since reliable records began in 1971. Two tropical cyclones – Cosme and Flossie – crossed into the central Pacific basin during the year, activity below the average of 4 to 5 systems.

<span class="mw-page-title-main">Hurricane Javier (2004)</span> Category 4 Eastern Pacific hurricane in 2004

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.

<span class="mw-page-title-main">Hurricane Paul (2006)</span> Category 2 Pacific hurricane in 2006

Hurricane Paul was a hurricane that ultimately struck Mexico as a tropical depression in October 2006. It developed from an area of disturbed weather on October 21, and 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 it reached its peak intensity 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.

<span class="mw-page-title-main">Tropical Storm Emilia (2006)</span> Pacific tropical storm in 2006

Tropical Storm Emilia was a rare tropical cyclone that affected the Baja California Peninsula in July 2006. The sixth tropical depression and fifth tropical storm of the 2006 Pacific hurricane season, it developed on July 21 about 400 miles (640 km) off the coast of Mexico. It moved northward toward the coast, reaching peak winds of 65 mph (105 km/h) before turning westward and encountering unfavorable conditions. Emilia later turned to the north, passing near Baja California as a strong tropical storm. Subsequently, the storm moved further away from the coast, and on July 27 it dissipated.

<span class="mw-page-title-main">2008 Pacific hurricane season</span> Hurricane season in the Pacific Ocean

The 2008 Pacific hurricane season was a near-average Pacific hurricane season which featured seventeen named storms, though most were rather weak and short-lived. Only seven hurricanes formed and two major hurricanes. This season was also the first since 1996 to have no cyclones cross into the central Pacific. The season officially began on May 15 in the eastern Pacific and on June 1 in the central Pacific. It ended in both regions on November 30. These dates, adopted by convention, historically describe the period in each year when most tropical cyclone formation occurs in these regions of the Pacific. This season, the first system, Tropical Storm Alma, formed on May 29, and the last, Tropical Storm Polo, dissipated on November 5.

<span class="mw-page-title-main">Hurricane Henriette (2007)</span> Category 1 Pacific hurricane in 2007

Hurricane Henriette was a minimal Category 1 hurricane that affected portions of Mexico in late August and early September 2007. The storm, which caused nine fatalities, formed from an area of disturbed weather on August 30, 2007, and became a tropical storm the next day. The cyclone moved parallel to the Mexican Pacific coast, but its proximity to the shore resulted in heavy rainfall over land. The most affected city was Acapulco, Guerrero, where six people were killed by landslides, and where over 100 families had to be evacuated after the La Sabana River flooded. Henriette then turned north and headed towards the Baja California peninsula, and became a Category 1 hurricane on the Saffir-Simpson Hurricane Scale. Henriette made its first landfall east of Cabo San Lucas at peak intensity, causing the death of one woman due to high surf.

<span class="mw-page-title-main">Tropical Storm Norman (2006)</span> Pacific tropical storm in 2006

Tropical Storm Norman was a weak tropical cyclone that brought heavy rainfall to southwestern Mexico in October 2006. The fifteenth named storm of the 2006 Pacific hurricane season, Norman developed on October 9 from a tropical wave well to the southwest of Mexico. Unfavorable conditions quickly encountered the system, and within two days of forming, Norman dissipated as its remnants turned to the east. Thunderstorms gradually increased again, as it interacted with a disturbance to its east, and on October 15 the cyclone regenerated just off the coast of Mexico. The center became disorganized and quickly dissipated, bringing a large area of moisture which dropped up to 6 inches (150 mm) of rainfall to southwestern Mexico. Rainfall from the storm flooded about 150 houses, of which 20 were destroyed. One person was injured, and initially there were reports of two people missing due to the storm; however, it was not later confirmed.

<span class="mw-page-title-main">2006 Pacific hurricane season</span> Hurricane season in the Pacific Ocean

The 2006 Pacific hurricane season was the first above-average season since 1997 which produced twenty-five tropical cyclones, with nineteen named storms, though most were rather weak and short-lived. Only eleven hurricanes formed and six major hurricanes. Following the inactivity of the previous seasons, forecasters predicted that season would be only slightly above active. It was also the first time since 2003 in which at least one cyclone of tropical storm intensity made landfall. The season officially began on May 15 in the East Pacific Ocean, and on June 1 in the Central Pacific; they ended on November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Pacific basin. However, the formation of tropical cyclones is possible at any time of the year.

<span class="mw-page-title-main">Hurricane Norbert (2008)</span> Category 4 Pacific hurricane in 2008

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.

<span class="mw-page-title-main">2009 Pacific hurricane season</span> Hurricane season in the Pacific Ocean

The 2009 Pacific hurricane season was the most active Pacific hurricane season since 1997. The season officially started on May 15 in the East 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 Pacific basin. The first tropical cyclone to form was One-E on June 18, and the last, Hurricane Neki, dissipated on October 27.

<span class="mw-page-title-main">Hurricane Raymond (1989)</span> Category 4 Pacific hurricane in 1989

Hurricane Raymond was the strongest tropical cyclone of the 1989 Pacific hurricane season, peaking as a strong Category 4 hurricane on the Saffir–Simpson hurricane scale. Forming out of a tropical wave on September 25, 1989, the tropical depression slowly tracked northwest before becoming nearly stationary the next day. Shortly after, the depression intensified into Tropical Storm Raymond and took a general westward track. Gradually intensifying, Raymond attained hurricane-status on September 28 and attained its peak intensity on September 30, with winds of 145 mph (233 km/h) and a barometric pressure of 935 mbar. Steady weakening then took place and by October 3, Raymond turned northeast towards land. The storm continued to weaken as it accelerated and eventually made landfall on the Baja California Peninsula as a tropical storm late on October 4 and a second landfall in Sonora, Mexico. Shortly after, Raymond weakened to a depression as it tracked inland. The remnants of the system persisted until October 7 when it dissipated over the Central United States.

<span class="mw-page-title-main">2013 Pacific hurricane season</span> Hurricane season in the Pacific Ocean

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.

<span class="mw-page-title-main">Tropical Storm Georgette (2010)</span> Pacific tropical storm in 2010

Tropical Storm Georgette was a short-lived tropical storm that struck Baja California Sur in September 2010. Georgette originated from an area of disturbed weather over the eastern Pacific ocean on September 20. The next day, the system was upgraded into a tropical storm a short distance south of Baja California Sur. As the storm moved over the peninsula, it weakened to a tropical depression. It continued north and as such made landfall on mainland Mexico on September 22. Georgette dissipated early the next day while located inland over Sonora. Although officials noted the threat for heavy rainfall across northwest Mexico and Baja California, damage was minimal and no deaths were reported in the country. However, remnant moisture moved into New Mexico, producing flooding that killed one person.

<span class="mw-page-title-main">2018 Pacific hurricane season</span> Hurricane season in the Pacific Ocean

The 2018 Pacific hurricane season was one of the most active Pacific hurricane seasons on record, producing the highest accumulated cyclone energy value on record in the basin. The season had the fourth-highest number of named storms – 23, tied with 1982. The season also featured eight landfalls, six of which occurred in Mexico. The season officially began on May 15 in the Eastern Pacific, 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 Pacific basin. However, tropical cyclone formation is possible at any time of the year, as illustrated when the first tropical depression formed on May 10, five days prior to the official start of the season.

<span class="mw-page-title-main">2020 Pacific hurricane season</span> Hurricane season in the Pacific Ocean

The 2020 Pacific hurricane season was the least active Pacific hurricane season since 2011. Altogether, 21 tropical cyclones developed. The season was near average in terms of tropical storms, featuring a total of 17, but had a well below average number of hurricanes and major hurricanes, with only 4 hurricanes and 3 major hurricanes forming. Additionally, no tropical cyclones formed in the Central Pacific basin for the first time since 2017, marking the start of a series of seasons with no tropical cyclogenesis occurring there. The season officially began on May 15 in the East 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 the respective regions. However, the formation of tropical cyclones is possible at any time of the year, as illustrated in 2020 by the formation of the season's first system, Tropical Depression One-E, on April 25. This the earliest formation of a tropical cyclone on record in the eastern Pacific basin proper.

<span class="mw-page-title-main">Hurricane Rosa (2018)</span> Category 4 Pacific hurricane

Hurricane Rosa brought widespread flooding to northwestern Mexico and the Southwestern United States in late September 2018, and was the first tropical cyclone to make landfall in Baja California since Nora in 1997. The seventeenth named storm, tenth hurricane, and seventh major hurricane of the 2018 Pacific hurricane season; Rosa originated from an Atlantic tropical wave that crossed the West African coast on September 6. The wave proceeded westward across the Atlantic, traversing Central America before entering the Gulf of Tehuantepec on September 22. There, the weather system acquired cyclonic features and became a tropical storm on September 25. Within a favorable atmosphere, Rosa entered a period of rapid intensification on September 27, peaking as a Category 4 hurricane with maximum sustained winds of 150 mph (240 km/h) a day later. Over the next few days, Rosa turned north and then northeast while steadily weakening, making landfall in Baja California as a tropical depression on October 2. After crossing over into the Gulf of California, the remnant system split apart and merged with an upper-level low off the coast of California by October 3.

<span class="mw-page-title-main">Hurricane Dolores (2015)</span> Category 4 Pacific hurricane in 2015

Hurricane Dolores was a powerful and moderately damaging tropical cyclone whose remnants brought record-breaking heavy rains and strong winds to California. The seventh named storm, fourth hurricane, and third major hurricane of the record-breaking 2015 Pacific hurricane season, Dolores formed from a tropical wave on July 11. The system gradually strengthened, attaining hurricane status on July 13. Dolores rapidly intensified as it neared the Baja California peninsula, finally peaking as a Category 4 hurricane on the Saffir–Simpson scale with winds of 130 mph (215 km/h) on July 15. An eyewall replacement cycle began and cooler sea-surface temperatures rapidly weakened the hurricane, and Dolores weakened to a tropical storm two days later. On July 18, Dolores degenerated into a remnant low west of the Baja California peninsula.

References

  1. 1 2 3 4 5 Robbie Berg (2008-12-02). "Tropical Cyclone Report: Tropical Storm Lowell" (PDF). National Hurricane Center. Retrieved 2009-02-19.
  2. Schauer Clark (2008). "Tropical Weather Discussion 0950 UTC September 5, 2008". National Hurricane Center. Retrieved 2008-10-11.[ permanent dead link ]
  3. Cab (2008). "Tropical Weather Discussion 1534 UTC September 5, 2008". National Hurricane Center. Retrieved 2008-10-11.[ permanent dead link ]
  4. John Brown (2008-09-04). "TROPICAL WEATHER OUTLOOK 500 PM PDT THU SEP 4 2008". National Hurricane Center. Retrieved 2009-03-11.
  5. Stacey Stewart (2008-09-06). "Tropical Depression LOWELL DISCUSSION NUMBER 1". National Hurricane Center. Retrieved 2009-03-11.
  6. James Franklin (2008-09-07). "Tropical Depression LOWELL DISCUSSION NUMBER 2". National Hurricane Center. Retrieved 2009-03-11.
  7. Rhome (2008-09-09). "Tropical Depression Lowell Discussion 11". National Hurricane Center. Retrieved 2009-03-11.
  8. John Brown (2008-09-10). "Tropical Depression LOWELL DISCUSSION NUMBER 14". National Hurricane Center. Retrieved 2009-03-11.
  9. Blake/Knabb (2008-09-10). "Tropical Depression LOWELL DISCUSSION NUMBER 17". National Hurricane Center. Retrieved 2009-03-11.
  10. Blake (2008-09-11). "Tropical Depression LOWELL DISCUSSION NUMBER 21". National Hurricane Center. Retrieved 2009-03-11.
  11. "Tormenta tropical 'Lowell' activa alerta en el Pacífico" (in Spanish).
Tropical Storm Lowell
Lowell 2008-09-09 1820Z.jpg
Lowell of the Mexican coast on September 9