Meteorological history | |
---|---|
Formed | November 23,2015 |
Remnant low | November 28,2015 |
Dissipated | November 29,2015 |
Category 4 major hurricane | |
1-minute sustained (SSHWS/NWS) | |
Highest winds | 150 mph (240 km/h) |
Lowest pressure | 934 mbar (hPa);27.58 inHg |
Overall effects | |
Fatalities | 4 total |
Damage | Minimal |
Areas affected | Central America,Western and Northwestern Mexico |
IBTrACS / [1] | |
Part of the 2015 Pacific hurricane season |
Hurricane Sandra was the latest-forming major hurricane in the northeastern Pacific basin, [nb 1] 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 (hPa;27.58 inHg) 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.
As the precursor to Sandra traversed Central America,it produced unseasonably heavy rainfall that triggered flooding and landslides. Four people died in various incidents related to the system:three in El Salvador and one in Honduras. Initially expecting a landfalling storm,officials in Northwestern Mexico prepared equipment for power outages,closed schools,and evacuated 180 residents. Sandra's effects largely consisted of light to moderate rainfall;some traffic accidents and landslides resulted from this,though the overall impacts were limited.
On November 6, 2015, a tropical wave emerged off the west coast of Africa into the Atlantic Ocean. Only sporadic convection—shower and thunderstorm activity—accompanied the system as it traveled west for the next ten days. As it reached the southwestern Caribbean on November 17, westerly winds associated with the Intertropical Convergence Zone spurred the development of an area of low pressure and extensive convection. [1] Forecasters at the National Hurricane Center (NHC) noted potential for the system to develop into a tropical cyclone; [2] however, persistent wind shear inhibited this system from consolidating before it reached Central America. The system emerged over the Pacific Ocean near Nicaragua on November 21; once back over water, convection blossomed near the low's center. [1] Convection remained largely disorganized over the following two days as the system progressed westward in response to a subtropical ridge to the north. [3]
A Tehuantepec gap wind event in conjunction with horizontal wind shear spurred development of a vortex within the disturbance and a well-defined low formed by 12:00 UTC on November 23. [1] Six hours later the low acquired sufficient convective organization, including elongated banding features to the north, [4] to be classified Tropical Depression Twenty-Two-E. At this time, the depression was situated 435 mi (705 km) south-southwest of Acapulco, Mexico. [1] Aided by high sea surface temperatures of 86 °F (30 °C), ample ocean heat content and low wind shear, the small system quickly intensified into a tropical storm—at which time the NHC assigned it the name Sandra—and developed a central dense overcast. [1] [5] [6] A prominent banding feature with cloud tops below −112 °F (−80 °C) and frequent lightning formed north of the circulation on November 24. [7] By 18:00 UTC, a 23 to 29 mi (37 to 47 km) wide eye became apparent, signaling the onset of rapid intensification. [1]
Throughout November 25, Sandra dramatically strengthened as deep convection blossomed around a tightening and clearing eye. [1] [8] The system achieved hurricane status by 06:00 UTC and major hurricane status—Category 3 or higher on the Saffir–Simpson hurricane wind scale—by 00:00 UTC on November 26. Prominent outflow became established atop the cyclone and further aided the intensification. [1] Throughout the strengthening phase, a mid- to upper-level trough near the west coast of North America created a weakness in the subtropical ridge, prompting Sandra to turn north around the western edge of the high. [1] [9] Sandra reached its peak intensity as a high-end Category 4 hurricane around 06:00 UTC on November 26 with maximum sustained winds of 150 mph (240 km/h) and a barometric pressure of 934 mbar (hPa; 27.58 inHg). By this time, the hurricane's eye shrunk to less than 6 mi (10 km) in diameter. [1] Within hours, however, increasing wind shear began to impact the circulation and caused convection to become asymmetric. Concurrently, the system started a turn northeast toward mainland Mexico as it rounded the ridge. [10]
Steadily increasing wind shear gradually unraveled Sandra during the latter part of November 26 and into November 27. [1] The storm's outflow, though prominent to the north, became restricted on the southern side. [11] Sandra briefly regained organization around 00:00 UTC on November 27, with its eye becoming redefined; however, persistent shear prevailed and the system weakened below major hurricane status by 06:00 UTC. [1] [12] The hurricane rapidly deteriorated throughout November 27 as convection became displaced to the northeast of the circulation. [13] The low-level circulation soon decoupled from the mid- to upper-level circulations and Sandra degraded to a tropical storm by 00:00 UTC on November 28. [1] [14] The convectively devoid low-level circulation abruptly turned northwest in response to a shallow ridge. Failing to redevelop convection atop its center, Sandra degenerated into a remnant low by 06:00 UTC. Sustained winds dropped below gale-force by 18:00 UTC. Intense thunderstorm activity did blossom to the northeast of the center late on November 28, prompting the storm to resume a northeasterly course. Sandra's remnants eventually succumbed to strong shear and opened up into a trough, roughly 60 mi (95 km) southwest of Culiacán, Mexico, late on November 29. [1]
Reaching tropical storm status on November 24, Sandra was the fourth-latest forming tropical storm in the Northeastern Pacific basin since reliable records began. [15] Upon becoming a hurricane at 06:00 UTC on November 25, Sandra was the second-latest such storm on record in the Northeastern Pacific; only Hurricane Winnie of 1983—the only December hurricane on record in the basin—formed later. [16] [17] This also marked the record-tying 16th hurricane to form in the Pacific north of the equator and east of the International Date Line; this record is shared with 1990, 1992, and 2014. [16] When it further became a major hurricane at 00:00 UTC on November 26, Sandra was the latest-forming such storm in the Northeastern Pacific basin on record. It surpassed the previous record set by Hurricane Kenneth in 2011 by nearly four days. [1] [18] Sandra was also the ninth major hurricane in the Northeastern Pacific proper and the eleventh east of the dateline, both setting a record for the most in a single season. [16] [19] Sandra's peak intensity with winds of 150 mph (240 km/h) and pressure of 934 mbar (hPa; 27.58 inHg) ranked it as the strongest November hurricane on record in the Northeastern Pacific, surpassing Hurricane Kenneth's 145 mph (230 km/h) and 940 mbar (hPa; 27.76 inHg). [1] [18] On a global scale, Sandra was the 30th major hurricane and "record-shattering" 25th Category 4 or 5 storm of 2015; the previous records were 23 and 18, respectively, occurring in both 1997 and 2004. [17] [20]
The precursor to Sandra produced unseasonably heavy rains across parts of Central America, leading to flooding. In Nicaragua, flooding affected 55 homes and destroyed 1, primarily in Managua. A total of 56 families required evacuation. Local officials blamed the flooding on trash-clogged drains. Five people were injured in the Nueva Segovia Department when an ambulance crashed on a foggy, rain-slicked road. [21] A landslide in Cucuyagua, Honduras, destroyed a home killing a 25-day-old baby and injuring four others. [22] In Nueva Esparta, El Salvador, two people drowned after being swept away by the swollen El Amatal River. Flooding in Ozatlán killed one person and inundated homes in Jiquilisco, prompting the evacuation of 14 families. [23]
Moisture from Sandra streamed northward into the Southern Plains and Lower Mississippi River Valley and contributed to widespread rainfall and flooding. [24] [25] Heavy rains affected portions of Texas, Oklahoma, Arkansas, Mississippi, and Tennessee. The Dallas–Fort Worth metroplex received 3.45 in (88 mm) of rain on November 27, their wettest November day on record; this total contributed to breaking the city's wettest-year on record. [20]
On November 26, the Government of Mexico issued a tropical storm watch for Baja California Sur between Todos los Santos and Los Barriles; this was discontinued less than 24 hours later. [1] The State Council of Civil Protection of Baja California Sur opened four shelters in both Cabo San Lucas and San José del Cabo; school officials cancelled classes for November 27. [26] In La Paz, the Federal Electricity Commission deployed 96 trucks to handle potential power outages. [27] On November 27, a tropical storm warning was raised for mainland Mexico between Altata and San Blas as well as the Islas Marías; the warning was discontinued the following day as Sandra rapidly dissipated. [1] Alerts were raised across portions of Sinaloa and Nayarit in advance of the hurricane. The port of Mazatlán suspended operations on November 28 and public shelters were opened in the city. [28] Water pumps, generators, and relief crews were mobilized at the port. [29] About 180 people from the small community of Boca Camichin, Nayarit, evacuated inland. The storm also prompted delay of the annual Maratón Pacífico. [28]
On November 27, Sandra produced wind gusts up to 40 mph (65 km/h) on Socorro Island as the storm moved 115 mi (185 km) southeast of the island. Effects from Sandra were minor and limited due to its dissipation offshore; rainfall was limited to 1 to 3 in (25 to 76 mm) in most areas and largely considered beneficial. [1] In contrast to predictions of 3.0 to 5.9 in (75 to 150 mm) of rain across Baja California Sur, only 0.71 in (18 mm) fell in San José del Cabo while other areas of the Los Cabos Municipality received a trace to no accumulation. [30] Wet roads in Cabo San Lucas resulted in two accidents that left three people injured. [31] In Chihuahua, minor landslides damaged roads. [32] [33]
The 2004 Pacific hurricane season was an overall below-average Pacific hurricane season in which there were 12 named tropical storms, all of which formed in the eastern Pacific basin. Of these, 6 became hurricanes, and 3 of those intensified into major hurricanes. No storms made landfall in 2004, the first such occurrence since 1991. In addition to the season's 12 named storms, there were five tropical depressions that did not reach tropical storm status. One of them, Sixteen-E, made landfall in northwestern Sinaloa. The season officially began on May 15 in the eastern Pacific, and on June 1 in the central Pacific basin. It officially ended in both basins on November 30. These dates conventionally delimit the period during each year when most tropical cyclones form in each respective basin. These dates conventionally delimit the period during each year when a majority of tropical cyclones form. The season was reflected by an accumulated cyclone energy (ACE) index of 71 units.
The 2005 Pacific hurricane season was a near-average Pacific hurricane season which produced fifteen named storms, seven hurricanes and two major hurricanes. It was also the second consecutive season in which no tropical cyclone of at least 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.
The 2003 Pacific hurricane season was the first season to feature no major hurricanes since 1977. The season officially began on May 15, 2003 in the Eastern North Pacific, and on June 1 in the Central ; both ended on November 30. These dates, adopted by convention, historically describe the period in each year when most tropical cyclogenesis occurs in these regions of the Pacific. The season featured 16 tropical storms, 7 of which intensified into hurricanes, which was then considered an average season. Damage across the basin reached US$129 million, and 23 people were killed by the storms.
The 1993 Pacific hurricane season included more than double the average number of major hurricanes – Category 3 or stronger cyclones on the Saffir–Simpson scale. This activity was the result of an El Niño event, which is the main factor contributing to above-average activity across the Pacific basin. The season featured 15 named storms, 11 hurricanes, and 9 major hurricanes. While the number of named storms was near the long-term average, the number of hurricanes was above the average of 8, and the number of major hurricanes far exceeded the long-term average of 4. Seasonal activity began on May 17 and ended on November 8, within the confines of a traditional hurricane season which begins on May 15 in the East Pacific and June 1 in the Central Pacific. The season ends on November 30 in both basins. These dates conventionally delimit the period during each year when most tropical cyclones form.
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 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 storms became hurricanes, of which two intensified into 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.
The 2011 Pacific hurricane season was a below average season in terms of named storms, although it had an above average number of hurricanes and major hurricanes. During the season, 13 tropical depressions formed along with 11 tropical storms, 10 hurricanes and 6 major hurricanes. The season officially began 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 season's first cyclone, Hurricane Adrian formed on June 7, and the last, Hurricane Kenneth, dissipated on November 25.
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.
The 2013 Pacific hurricane season was an above average Pacific hurricane season with 21 tropical cyclones forming. Of these, 20 became named storms – 18 in the Eastern Pacific basin, and 2 in the Central Pacific basin. Of the 18 named storms in the east, 9 became hurricanes, with one, Raymond, becoming the season's only major hurricane. In the central, neither named storm became a hurricane. It was also a below-normal season in terms of Accumulated cyclone energy (ACE), as many of its systems 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 development occurs in these North Pacific basins. The first cyclone, Tropical Storm Alvin, formed on May 15, and the last, Tropical Storm Sonia, dissipated on November 4.
The 2014 Pacific hurricane season was one of the busiest and costliest Pacific hurricane seasons since the keeping of reliable records began in 1949. 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 these regions of the Pacific.
The 2015 Pacific hurricane season is the second-most active Pacific hurricane season on record, with 26 named storms, only behind the 1992 season. A record-tying 16 of those storms became hurricanes, and a record 11 storms further intensified into major hurricanes throughout the season. The Central Pacific, the portion of the Northeast Pacific Ocean between the International Date Line and the 140th meridian west, had its most active year on record, with 16 tropical cyclones forming in or entering the basin. Moreover, the season was the third-most active season in terms of accumulated cyclone energy, amassing a total of 290 units. The season officially started 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 Northeast Pacific basin. However, the formation of tropical cyclones is possible at any time of the year. This was shown when a tropical depression formed on December 31. The above-average activity during the season was attributed in part to the very strong 2014–2016 El Niño event.
The 2016 Pacific hurricane season was tied as the fifth-most active Pacific hurricane season on record, alongside the 2014 season. Throughout the course of the year, a total of 22 named storms, 13 hurricanes and six major hurricanes were observed within the basin. Although the season was very active, it was considerably less active than the previous season, with large gaps of inactivity at the beginning and towards the end of the season. It officially started 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 these regions of the Pacific Ocean. However, tropical development is possible at any time of the year, as demonstrated by the formation of Hurricane Pali on January 7, the earliest Central Pacific tropical cyclone on record. After Pali, however, no tropical cyclones developed in either region until a short-lived depression on June 6. Also, there were no additional named storms until July 2, when Tropical Storm Agatha formed, becoming the latest first-named Eastern Pacific tropical storm since Tropical Storm Ava in 1969.
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.
Hurricane Carlos was an unusually small tropical cyclone which affected the western coast of Mexico in June 2015. Forming as the third named storm and hurricane of the annual hurricane season, Carlos developed from a trough first noted by the National Hurricane Center on June 7. The disturbance gradually organized and was designated as a tropical depression three days later while south of the Mexican Pacific coast. Drifting slowly northwestward, the depression was upgraded further to a tropical storm. Although persistent wind shear and dry air hampered intensification early on, Carlos strengthened into a hurricane on June 13 after moving into a more favorable environment. However, the return of dry air and upwelling of cooler waters caused the system to deteriorate into a tropical storm. Paralleling the Mexican coast, Carlos later regained hurricane intensity on June 15 and attained peak winds of 90 mph (140 km/h) a day later. The reprieve was brief, however, as the onset of wind shear, land interaction, and dry air afterward led to rapid weakening. On June 17, Carlos degenerated into a remnant area of low pressure, having made landfall in Jalisco earlier that day. By the morning of June 18, Carlos was declared to have completely dissipated.
The 2019 Pacific hurricane season was an above average season which produced nineteen named storms, most of which were rather weak and short-lived. Only seven hurricanes formed, the fewest since 2010. The season officially began 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. This season was one of the latest-starting Pacific hurricane seasons on record, with the first tropical cyclone, Hurricane Alvin, forming on June 25. The final system, Tropical Depression Twenty-One-E, dissipated on November 18.
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