Hurricane Nate (2005)

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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

A tropical wave emerged from the west coast of Africa on August 30 and tracked westward across the Atlantic Ocean, maintaining a vigorous area of convection along the wave axis. By September 1 most of the deep convection had been stripped away by southwesterly wind shear. Despite this, the wave remained well-defined as it continued west-northwest. The wave split into two pieces; the northern portion passed between the Leeward Islands and Hurricane Maria on September 3, while the southern portion moved into the Caribbean Sea. On September 4, the northern portion of the wave began to interact with an upper-level low pressure system and an elongated trough that was located between Bermuda and the Leeward Islands [1] —the same trough which contributed to the development of Hurricane Ophelia. [2] As a result of the low wind shear, convection redeveloped and organized along the wave axis. Convective banding formed around a broad surface low. It is estimated that the system developed into a tropical depression at 1800  UTC on September 5. At the time it was located approximately 350 miles (560 km) to the south-southwest of Bermuda. [1]

Upon being designated, Tropical Depression Fifteen developed deep convection close to, and to the east of, the center of circulation. At the same time, banding features became better organized. [3] Later on September 5, the overall cloud pattern improved while thunderstorm activity condensed and deepened within the increasingly well-defined circulation. [4] Just six hours after being designated as a tropical depression, the cyclone intensified into a tropical storm; it was given the name Nate by the National Hurricane Center. Over the following two days, Nate drifted slowly northeastward towards Bermuda. [1]

Within the early hours of September 6, Nate became quasi-stationary under a weak steering pattern between Hurricane Maria and a disturbance over The Bahamas. [5] Satellite imagery indicated that the cloud pattern continued to organize with excellent outflow surrounding the storm. [6] Late on September 6 a developing banding eye feature became evident. [7] Tropical Storm Nate strengthened further and became a hurricane at 1200 UTC on September 7, as it began to turn away from Bermuda. [1] Some models indicated that Nate could have been either absorbed by or merged with the larger Hurricane Maria, but the National Hurricane Center (NHC) forecast that Nate would survive as a separate system, which it did. [8] The large low to the northeast of The Bahamas gradually opened into a broad trough as a shortwave trough approached from the northwest. The larger trough slowly became elongated in a northeast–southwest manner late on September 7. At the same time, the shortwave trough moved southward along the west side of the other trough. The increasing southwesterly flow along the southeast side of the broad trough caused Nate to accelerate northeastward. Nate reached its peak intensity of 90 mph (145 km/h) late on September 8 as it passed 120 miles (205 km) southeast of Bermuda, while its strongest winds remained well offshore. [1]

While at peak intensity, the storm maintained a well-organized and "impressive" convective pattern. [9] Soon after the storm peaked in strength, increasing wind shear and dry air caused Nate to weaken back into a tropical storm later on September 9. [1] Satellite imagery showed that the cloud pattern began to rapidly deteriorate. [10] The hurricane was downgraded to a tropical storm at 1800 UTC on September 9 and continued to weaken as wind shear increased in association with an approaching trough and a related cold front. [1] By late on September 9, all of the already limited convective activity was confined to the eastern semicircle, leaving the low-level center exposed. [11] The storm was reduced to a swirl of low-level clouds just hours later. [12] Nate became extratropical the next day before becoming absorbed by a larger system by 0000 UTC on September 13, to the north-northeast of the Azores. [1]

Impact, records, and naming

Tropical Storm Nate intensifying on September 6 Hurricane Nate Sept 6 05.jpg
Tropical Storm Nate intensifying on September 6

A tropical storm watch was issued for Bermuda early on September 7, and later that day a tropical storm warning and a hurricane watch superseded it. However, the storm did not reach the island, so the warnings were canceled as the storm moved away September 8. [1] Four cruise ships left the island ahead of schedule, and flights were canceled in anticipation of Nate. [13] [14]

The outer bands of Nate brushed Bermuda with sustained winds of 35 mph (55 km/h) and widespread showers. [1] [15] Gusts were higher, peaking at roughly 50 mph (80 km/h). [16] Less than 1 inch (25 mm) of rain was recorded at Bermuda International Airport. [1] Damage in Bermuda was minimal. [1] Two ships reported tropical storm-force winds in association with the storm: the Maersk New Orleans, to the north of the storm's center, and a ship with the call sign WCZ858 to the east-southeast. [1] Rip currents from Nate and the more distant Maria killed one and injured another in New Jersey; several others were caught in rip currents, though they were able to escape. [17] In the Carolinas, Nate also contributed to heightened seas, though this time in combination with Hurricane Ophelia and persistent unrelated northeasterly winds. A buoy just offshore Cape Fear recorded waves up to 12 ft (3.7 m). [18]

Tropical energy from the remnants of Nate and Maria merged to form a broad storm system that would track toward parts of Europe. The mid-latitude cyclone produced a day of heavy rains across the Scottish Highlands that included a 24-hour precipitation total of 5.17 in (131 mm) on the Isle of Skye. [19] As it continued north, the storm also dropped torrential rainfall over Western Norway. The region suffered extensive flooding and mudslides, including one that killed one person and injured nine more. [19] [20] Although the remnants of Nate and Maria avoided England, they broke a streak of above-average temperatures in the region, filtering down much cooler Arctic air. In places, this led to the first frost of the winter season. [21] Temperatures down to −1.7 °C (28.9 °F) were recorded following the influx of colder air, with readings below freezing as far south as Hertfordshire. [19]

Four Canadian Navy ships headed to the Gulf Coast of the United States, carrying relief supplies to help in the aftermath of Hurricane Katrina, were slowed down trying to avoid Hurricanes Nate and Ophelia. [22] The convoy included a destroyer, two frigates, and an icebreaker, and developed a plan to travel between the two hurricanes to minimize damage to their cargo. Anticipating rough seas and gusty winds even with the altered course, crews secured onboard supplies which included generators, chainsaws, diapers, and cots. [23] The genesis of Tropical Storm Nate continued the unprecedented levels of tropical activity during the 2005 hurricane season; when it developed on September 5, it was the earliest in any season that the fourteenth named tropical cyclone formed, surpassing the previous record held by an unnamed storm during the 1936 season. This record was later broken in 2020 when Tropical Storm Nana formed on September 1, four days earlier. [24]

See also

Related Research Articles

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<span class="mw-page-title-main">2002 Atlantic hurricane season</span>

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<span class="mw-page-title-main">2005 Atlantic hurricane season</span>

The 2005 Atlantic hurricane season was the most active on record in terms of number of tropical cyclones, until surpassed by the 2020 season. It featured 28 tropical or subtropical storms. The United States National Hurricane Center named 27 storms, exhausting the annual pre-designated list, requiring the use of six Greek letter names, and adding an additional unnamed storm during a post-season re-analysis. A record 15 storms attained hurricane status, with maximum sustained winds of at least 74 miles per hour (119 km/h). Of those, a record seven became major hurricanes, rated Category 3 or higher on the Saffir–Simpson scale. Four storms of this season became Category 5 hurricanes, the highest ranking.

<span class="mw-page-title-main">Hurricane Ophelia (2005)</span> Category 1 Atlantic hurricane in 2005

Hurricane Ophelia was a long-lived tropical cyclone in September 2005 that moved along an erratic path off the East Coast of the United States for much of its existence. The fifteenth named storm and the eighth hurricane of the record-breaking 2005 Atlantic hurricane season, Ophelia originated from a complex set of systems across the Atlantic in early September. An area of low pressure consolidated near the Bahamas and was classified as Tropical Depression Sixteen on September 6. Stuck in a region of meager steering currents, largely dominated by a lull between two ridges to the north and east, this system moved along a looping course with a general northward trajectory. The following day it organized into Tropical Storm Ophelia and soon reached hurricane status on September 8. Over the next week, Ophelia's intensity oscillated between tropical storm and hurricane levels due to intrusions of dry air, varying levels of wind shear, and gradual upwelling of cooler waters along its meandering path. Gradually growing in size, the system reached hurricane strength for the fourth time and its peak strength on September 14, with maximum sustained winds of 85 mph (140 km/h). By this time Ophelia had completed a second loop and was moving northwest toward North Carolina. Changing direction once again, the system turned away from the state though its eyewall scraped the coastline for two days. The system degraded to tropical storm strength for a final time on September 16 as it began accelerating northeast. Becoming embedded within the westerlies, Ophelia transitioned into an extratropical cyclone the next day. Remaining on a steady east-northeast to northeast path for the next week, Ophelia traversed Atlantic Canada and the northern Atlantic Ocean before dissipating on September 23 over the Norwegian Sea.

<span class="mw-page-title-main">Tropical Storm Ana (2003)</span> Atlantic tropical storm

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<span class="mw-page-title-main">Hurricane Gert (1999)</span> Category 4 Atlantic hurricane in 1999

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<span class="mw-page-title-main">Hurricane Erin (2001)</span> Category 3 Atlantic hurricane

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<span class="mw-page-title-main">Tropical Storm Edouard (2002)</span> Atlantic tropical cyclone

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<span class="mw-page-title-main">Hurricane Olga</span> Category 1 Atlantic hurricane in 2001

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<span class="mw-page-title-main">Tropical Storm Gabrielle (2007)</span> Atlantic tropical cyclone

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<span class="mw-page-title-main">Hurricane Isaac (2000)</span> Category 4 Atlantic hurricane in 2000

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<span class="mw-page-title-main">Hurricane Bertha (2008)</span> Category 3 Atlantic hurricane in 2008

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<span class="mw-page-title-main">Tropical Storm Kiko (2007)</span> Pacific tropical cyclone

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

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. There were eleven hurricanes, of which six became 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 one 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.

<span class="mw-page-title-main">Meteorological history of Hurricane Gustav</span>

The meteorological history of Hurricane Gustav spanned eleven days, from August 25 to September 4, 2008. The tropical disturbance which eventually spawned Hurricane Gustav gathered on August 16, southwest of the Cape Verde islands, but was slow to develop as it trekked west across the Atlantic. Upon reaching the warm waters of Caribbean Sea it began to organize and became a tropical depression on August 25. It quickly strengthened to a tropical storm, and then a hurricane, before making landfall on Haiti's southwest peninsula. Gustav was severely disrupted by Hispaniola's mountains and stalled, disorganized, in the Gulf of Gonâve between August 26 and 27.

<span class="mw-page-title-main">2011 Atlantic hurricane season</span>

The 2011 Atlantic hurricane season was the second in a group of three very active Atlantic hurricane seasons, each with 19 named storms, tied with 1887, 1995, 2010, and 2012. The above-average activity was mostly due to a La Niña that persisted during the previous year. Of the season's 19 tropical storms, only seven strengthened into hurricanes, and four of those became major hurricanes: Irene, Katia, Ophelia, and Rina. The season officially began on June 1 and ended on November 30, dates which conventionally delimit the period during each year in which most tropical cyclones develop in the Atlantic Ocean. However, the first tropical storm of the season, Arlene, did not develop until nearly a month later. The final system, Tropical Storm Sean, dissipated over the open Atlantic on November 11.

<span class="mw-page-title-main">Hurricane Maria (2011)</span> Category 1 Atlantic hurricane in 2011

Hurricane Maria was a Category 1 hurricane that made landfall on the island of Newfoundland during September 2011. Originating from a tropical wave over the central Atlantic on September 6, Maria moved toward the west and slowly strengthened. While approaching the northern Leeward Islands, however, the system entered a region of higher vertical wind shear and cooler sea surface temperatures, causing it to degenerate into a low-pressure area. It slowly curved toward the north and northeast around the western periphery of the subtropical ridge, and regained tropical storm status on September 10. Maria further strengthened to attain hurricane status while making its closest approach to Bermuda. The cyclone attained peak winds of 80 mph (130 km/h) on September 16, but weakened thereafter because of an increase in wind shear and cooler sea surface temperatures. Maria made landfall on the southeastern coast of Newfoundland during the afternoon hours of September 16 before becoming absorbed by a frontal system later on that same day.

<span class="mw-page-title-main">Hurricane Nadine</span> Category 1 Atlantic hurricane in 2012

Hurricane Nadine was an erratic Category 1 hurricane that became the fourth-longest-lived Atlantic hurricane on record. As the fourteenth tropical cyclone and named storm of the 2012 Atlantic hurricane season, Nadine developed from a tropical wave traveling west of Cape Verde on September 10. On the following day, it had strengthened into Tropical Storm Nadine. After initially tracking northwestward, Nadine turned northward, well away from any landmass. Early on September 15, Nadine reached hurricane status as it was curving eastward. Soon after, an increase in vertical wind shear weakened Nadine and by September 16 it was back to a tropical storm. On the following day, the storm began moving northeastward and threatened the Azores but late on September 19, Nadine veered east-southeastward before reaching the islands. Nonetheless, the storm produced tropical storm force winds on a few islands. On September 21, the storm curved south-southeastward while south of the Azores. Later that day, Nadine transitioned into a extratropical low pressure area.

<span class="mw-page-title-main">2017 Atlantic hurricane season</span>

The 2017 Atlantic hurricane season was a devastating and extremely active Atlantic hurricane season that became the costliest on record, with a damage total of at least $294.92 billion (USD). The season featured 17 named storms, 10 hurricanes, and 6 major hurricanes. Most of the season's damage was due to hurricanes Harvey, Irma, and Maria. Another notable hurricane, Nate, was the worst natural disaster in Costa Rican history. These four storm names were retired following the season due to the number of deaths and amount of damage they caused. Collectively, the tropical cyclones were responsible for at least 3,364 deaths. The season also had the highest accumulated cyclone energy (ACE) since 2005 with an approximate index of 224 units, with a record three hurricanes each generating an ACE of over 40: Irma, Jose, and Maria. This season featured two Category 5 hurricanes, and the only season other than 2007 with two hurricanes making landfall at that intensity. The season's ten hurricanes occurred one after the other, the greatest number of consecutive hurricanes in the satellite era, and tied for the highest number of consecutive hurricanes ever observed in the Atlantic basin.

<span class="mw-page-title-main">Hurricane Alex (2016)</span> Category 1 Atlantic hurricane

Hurricane Alex was the first Atlantic hurricane to occur in January since Hurricane Alice of 1954–55. Alex originated as a non-tropical low near the Bahamas on January 7, 2016. Initially traveling northeast, the system passed by Bermuda on January 8 before turning southeast and deepening. It briefly acquired hurricane-force winds by January 10, then weakened slightly before curving towards the east and later northeast. Acquiring more tropical weather characteristics over time, the system transitioned into a subtropical cyclone well south of the Azores on January 12, becoming the first North Atlantic tropical or subtropical cyclone in January since Tropical Storm Zeta of 2005–2006. Alex continued to develop tropical features while turning north-northeast, and transitioned into a fully tropical cyclone on January 14. The cyclone peaked in strength as a Category 1 hurricane on the Saffir–Simpson scale (SSHWS), with maximum sustained winds of 85 mph and a central pressure of 981 mbar. Alex weakened to a high-end tropical storm before making landfall on Terceira Island on January 15. By that time, the storm was losing its tropical characteristics; it fully transitioned back into a non-tropical cyclone several hours after moving away from the Azores. Alex ultimately merged with another cyclone over the Labrador Sea on January 17.

References

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  3. Robert Molleda and Richard Pasch (September 5, 2005). "Tropical Depression 15 Discussion Number 1". National Hurricane Center. Retrieved January 5, 2009.
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Hurricane Nate
Nate Sept 7 2005 1730Z (cropped).jpg
Hurricane Nate at peak intensity southeast of Bermuda on September 9