Hurricane Connie was a Category 4 hurricane that contributed to significant flooding across the eastern United States in August 1955, just days before Hurricane Diane affected the same general area. Connie formed on August 3 from a tropical wave in the eastern Atlantic Ocean. It moved quickly west-northwestward, strengthening into a hurricane by August 4. Connie first posed a threat to the Lesser Antilles, ultimately passing about 105 mi (169 km) north of the island group. In the United States Virgin Islands, three people died due to the hurricane, and a few homes were destroyed. The outer rainbands produced hurricane-force wind gusts and intense precipitation, reaching 8.65 in (220 mm) in Puerto Rico. On the island, Connie destroyed 60 homes and caused crop damage. After affecting Puerto Rico, Connie reached maximum sustained winds of 140 mph (230 km/h), and a barometric pressure of 944 mbar (27.9 inHg), as observed by the Hurricane Hunters on August 7. The hurricane later weakened, slowed its forward motion, and turned to the north, striking North Carolina on August 12 as a Category 2 on the Saffir-Simpson scale. Connie was the first of three damaging tropical cyclones in the 1955 hurricane season to hit the state, along with Diane and Ione. The storm progressed inland after moving through the Chesapeake Bay region, and was later absorbed by a cold front over Lake Huron on August 15.
The 1897 Atlantic hurricane season was an inactive season, featuring only six known tropical cyclones, four of which made landfall. There were three hurricanes, none of which strengthened into major hurricanes, which are Category 3 or higher on the modern-day Saffir–Simpson hurricane wind scale. The first system was initially observed south of Cape Verde on August 31, an unusually late date. The storm was the strongest of the season, peaking as a Category 2 hurricane with winds of 100 mph (155 km/h). While located well north of the Azores, rough seas by the storm sunk a ship, killing all 45 crewmen. A second storm was first spotted in the Straits of Florida on September 10. It strengthened into a hurricane and tracked northwestward across the Gulf of Mexico, striking Louisiana shortly before dissipating on September 13. This storm caused 29 deaths and $150,000 (1897 USD) in damage.
The Napier-Hastings Urban Area was defined by Statistics New Zealand as a main urban area of New Zealand that was based around the twin cities of Napier and Hastings in the Hawke's Bay Region. It was defined under the New Zealand Standard Areas Classification 1992 (NZSAC92), which has since been superseded by the Statistical Standard for Geographic Areas 2018 (SSGA18).
The Gale of 1878 was an intense Category 2 hurricane which caused extensive damage from Cuba to New England in October 1878. Believed to be the strongest storm to hit the Washington - Baltimore region since hurricane records began in 1851, a complete record exists of this hurricane from its formation to dissipation.
Hurricane Charley was the second hurricane to threaten the East Coast of the United States within a year's timeframe, after Hurricane Gloria of 1985. The third tropical storm and second hurricane of the season, Charley formed as a subtropical low on August 13 along the Florida panhandle. After moving off the coast of South Carolina, the system transitioned into a tropical cyclone and intensified into a tropical storm on August 15. Charley later attained hurricane status before moving across eastern North Carolina. It gradually weakened over the north Atlantic Ocean before transitioning into an extratropical cyclone on August 20. Charley's remnants remained identifiable for over a week, until after crossing Ireland and Great Britain they dissipated on August 30.
Hurricane Ella brought flooding to the Greater Antilles and Texas in September 1958. The fifth named storm and third hurricane of the annual season, Ella developed from a tropical wave located just east of the Lesser Antilles on August 30. Initially a tropical depression, it strengthened into Tropical Storm Ella six hours later. The system crossed the Leeward Islands and entered the Caribbean Sea late on August 30. Ella headed westward and by August 31, intensified into a Category 1 hurricane. Hours later, it strengthened into a Category 2 hurricane on the Saffir–Simpson hurricane wind scale. The storm curved northwestward while south of Hispaniola and as a result, struck the Tiburon Peninsula of Haiti on September 1. Flooding in that country killed 30 people in Aux Cayes and left 3 other missing. Additionally, thousands were left homeless, about one-third of crops were washed out, and numerous cattle were killed.
The 1933 Outer Banks hurricane lashed portions of the North Carolina and Virginia coasts less than a month after another hurricane hit the general area. The twelfth tropical storm and sixth hurricane of the 1933 Atlantic hurricane season, it formed by September 8 to the east of the Lesser Antilles. It moved generally to the north-northwest and strengthened quickly to peak winds of 140 mph (230 km/h) on September 12. This made it a major hurricane and a Category 4 on the Saffir-Simpson scale. The hurricane remained at or near that intensity for several days while tracking to the northwest. It weakened approaching the southeastern United States, and on September 16 passed just east of Cape Hatteras, North Carolina with winds of about 100 mph (160 km/h). Turning to the northeast, the hurricane became extratropical on September 18 before moving across Atlantic Canada, eventually dissipating four days later.
The 1927 Nova Scotia hurricane was the deadliest tropical cyclone striking Canada in the 20th century. The first observed storm of the season, this cyclone developed from a tropical wave over the deep tropics of the Atlantic Ocean on August 18. Initially a tropical storm, it moved west-northwestward and intensified into a Category 1 hurricane on the modern day Saffir–Simpson hurricane wind scale by August 19. The storm intensified significantly over the next few days, and by August 22, it peaked as a Category 3 hurricane with maximum sustained winds of 125 mph (205 km/h). Around that time, the system began curving northwestward and later northward. By August 23, it turned to the north-northeast and then began weakening on August 24. Thereafter, the storm accelerated toward Atlantic Canada. Late on August 24, the hurricane struck near Yarmouth, Nova Scotia, as a Category 2 hurricane, just before becoming extratropical.
The Hawke's Bay cricket team, representing the Hawke's Bay region of New Zealand, played first-class cricket between 1883–84 and 1920–21, and competed in the Plunket Shield in the 1914–15 and 1920–21 seasons. The side has continued to appear in minor cricket and now competes in the Hawke Cup competition, where it has been the dominant team from 2020 to 2024.
Waikokopu is a small coastal settlement in the north of New Zealand's Hawke's Bay Region, where the Waikokopu stream forms a small tidal estuary between two prominent headlands. The name Waikokopu translates from Māori as "waters" (wai) of the "kokopu", the kokopu being any one of three species of small native fresh-water fish. Waikokopu is about 40 km east of Wairoa, the largest town in northern Hawke's Bay.
The 1812 Louisiana Hurricane was a major hurricane that struck New Orleans, Louisiana, during the War of 1812. It was the worst storm of the early history of New Orleans and was very likely the hurricane which made the closest landfall known to affect the city.
The climate of New Zealand is varied due to the country's diverse landscape. Most regions of New Zealand belong to the temperate zone with a maritime climate characterised by four distinct seasons. Winters are relatively mild and summers comparatively cool. The main contributing factors are the Pacific Ocean and latitude, although the mountain ranges can cause significant climate variations in locations barely tens of kilometres from each other. Conditions vary from extremely wet on the West Coast of the South Island to almost semi-arid in Central Otago and subtropical in Northland.
Hurricane Josephine was a long-lived Atlantic hurricane that threatened the East Coast of the United States for several days in October 1984. The sixteenth tropical cyclone, tenth named storm, and third hurricane of the season, Josephine developed from an area of disturbed weather near the Bahamas on October 7, forming with subtropical characteristics. It quickly organized, and gained tropical characteristics as it strengthened into a tropical storm on October 8. Gradual intensification occurred thereafter, reaching hurricane status on October 10. The storm headed northward, remaining well offshore of the eastern United States. Josephine strengthened further and peaked as a moderately strong Category 2 hurricane on the Saffir-Simpson Hurricane Scale on October 12. On the following day, Josephine weakened back to a Category 1 hurricane before becoming nearly stationary. It later headed northeastward and paralleled the coast well offshore of Nova Scotia. By October 17, Josephine weakened back to a tropical storm, shortly before beginning to execute a cyclonic loop to the south of Newfoundland. While executing the cyclonic loop, Josephine became extratropical on October 18.
TSS Arahura was a twin screw steam passenger/cargo ship built for the Union Steam Ship Company. It was launched on the Clyde on 25 March 1905 and built by William Denny and Brothers Dumbarton at a cost of £52,000. It had a gross weight of 1,607 tons. The ship had accommodation for 201 passengers.
The 2013 New Zealand winter storm was a highly intense extratropical cyclone which affected New Zealand on 20–22 June. The storm brought strong winds and high waves especially around the Wellington Region, and further afield chilling cold temperatures and heavy snow to the South Island. The storm was described by the New Zealand National Institute of Water and Atmospheric Research (NIWA) as an extreme event. The maximum 10-minute average, sustained wind reading, recorded at Wellington airport was 101 km/hour, with individual gusts up to 130–140 km/hour at this location. Winds were equivalent to the strength of a category 1 or 2 hurricane on the Saffir–Simpson hurricane wind scale. Record wave heights of 15 m peak to trough were recorded by a buoy offshore from Baring Head in the Cook Strait. The highest wind gust was 202 km/h, at Mt Kaukau, Wellington.
The great storm of 1868 was a violent storm that swept across much of New Zealand between 1–6 February 1868, wrecking 12 ships – including the Star of Tasmania and Water Nymph at Oamaru – and causing extensive flooding. About 40 people are known to have died and at the time an estimated £500,000 to £1 million worth of damage was caused. The storm is currently thought to have been an extratropical cyclone, which peaked in New Zealand over the period between the 3rd and 4th. In total 2,585 tons of shipping was lost, which was nearly half the tonnage lost during the full year. The flooding in the south of the South Island was the worst until 1945. The loss of life among the Māori population, if any, was not known as many lived in isolated areas, newspaper reporting of the time was Eurocentric, and at the time internal conflict, the New Zealand Wars, was reaching its culmination.
The 1842 Atlantic hurricane season featured several maritime catastrophes in the Gulf of Mexico and along the U.S. East Coast, and produced one of the only known tropical cyclones to directly affect the Iberian Peninsula. As the season falls outside the scope of the Atlantic hurricane database, records of most storms in 1842 are scarce, and only approximate tracks are known. The first documented storm of the season battered the coast of North Carolina in mid-July, wrecking dozens of ships and destroying homes along the Outer Banks. A little over a month later, another storm impacted the same region and caused several more shipwrecks that killed at least 12 men. This storm later doused the Mid-Atlantic states with flooding rains. In early September, a powerful storm known as "Antje's Hurricane"—named after a ship that it dismasted—tracked generally westward after first being spotted over the Leeward Islands. After yielding widespread destruction across the Bahamas, the storm traversed the Florida Straits, causing severe damage in both northern Cuba and the lower Florida Keys. Many ships and their crews were lost to the storm as it crossed the Gulf of Mexico; it finally struck northern Mexico on September 8.
The 1936 New Zealand Cyclone was an unnamed tropical cyclone originating near the Solomon Islands that struck New Zealand on 1 February 1936 causing widespread flooding and destruction. The cyclone claimed at least 12 lives in New Zealand.
Hurricane San Roque was a destructive tropical cyclone in August 1893 that principally affected Puerto Rico, eastern New England, and Atlantic Canada. Its informal name in Puerto Rico arises from the feast day of Saint Roch, or San Roque in Spanish, which coincided with the hurricane's landfall on that island. It was the third known hurricane of the 1893 Atlantic hurricane season. The system was first observed on August 13 at low latitudes east of the Lesser Antilles. It grew to be a powerful, slow-moving hurricane in the Caribbean Sea, and on August 17 struck Puerto Rico at the equivalence of Category 3 on the modern-day Saffir–Simpson scale. The eye crossed the island from southeast to northwest in about seven hours. A prolonged period of strong winds caused widespread destruction on the island, most notably along the northern coast. Large numbers of homes sustained varying degrees of damage, with flimsy shacks belonging to poor workers faring the worst; many families were left homeless, and four people were killed. Telegraph communications were severed across the island. In addition to the intense winds, several days of heavy rainfall in interior sectors triggered extensive river flooding. The combined effects of rain and wind destroyed fields of crops, most notably coffee and sugar cane.
