7/8/2023 0 Comments Henri hurricane track![]() It’s just a tropical weather phenomenon, the National Weather Service says. Most tropical systems in the northern hemisphere run out or recur before they can make their way north, according to the National Weather Service. There are two ingredients needed for a storm to track this far up north: a tropical system itself and steering currents. WHAT ARE THE CONDITIONS NEEDED FOR AN HENRI (OR BOB OR GLORIA)? These storms have human names courtesy the World Meteorological Association, which draws up a list of 21 names for each Atlantic hurricane season. JE M’APPELLE HENRI - WHY DO I SHARE A NAME WITH A STORM? But with Connecticut in Henri’s path, some might better remember Gloria - the September 1985 hurricane made landfall on both Long Island and Connecticut and caused eight deaths and nearly $1 billion in damage. Bob was its predecessor, responsible for the deaths of 17 and $1.5 billion in damage in August 1991. Had it made landfall as a hurricane, it would have been New England’s first in 30 years. Henri had strengthened into a hurricane Saturday morning before losing steam Sunday. The storm surge - a wall of sea water pushed ahead of the storm by its winds - wasn’t significant like it was with 2012′s Superstorm Sandy, the effects of which are still plaguing New York.Ī stormy trio. Rain continued falling in some of those areas Monday, but cleanup was largely underway in New Jersey. It dropped to a tropical depression when sustained winds fell below 39 mph.Īfter coming ashore, Henri veered west, dumping large amounts of rain on Connecticut, New York’s Hudson River Valley, parts of New Jersey and even Pennsylvania. A tropical storm? 39-73 mph.Īs of Sunday evening, Henri’s sustained winds topped out at 40 mph (64 kph), well below hurricane status. The maximum sustained winds for a hurricane are anything above 74 mph. Retrieved January 14, 2008.It’s all about the wind. National Oceanic and Atmospheric Administration. Archived from the original on 6 December 2006. "Chronological Listing of Tropical Cyclones affecting North Florida and Coastal Georgia 1565-1899". ^ a b c d e Hurricane Research Division (2008). ![]() "Documentation of Atlantic Tropical Cyclones Changes in HURDAT". Diaz, 1995b "A Reconstruction of Historical Tropical Cyclone Frequency in the Atlantic from Documentary and other Historical Sources : 1851-1880 Part II: 1871-1880" Climate Diagnostics Center, NOAA, Boulder, CO Hurricanes and Typhoons: Past, Present and Future. "The Atlantic hurricane database re-analysis project: Documentation for the 1851–1910 alterations and additions to the HURDAT database". Systems Tropical Storm One Tropical storm (SSHWS) It crossed the Florida peninsula and hit South Carolina as a category 1 hurricane. The final storm of the season began as a tropical storm in the Gulf of Mexico on October 22. Growing from a tropical storm first seen south-west of the Cape Verde Islands, it traveled across the Atlantic and was last seen near the Azores on October 6. It traveled north and developed into a hurricane, but never made landfall and was last observed on September 19. Hurricane Three grew from a tropical storm that formed east of the Lesser Antilles. Hurricane Two, the strongest storm of the season, traveled across the Atlantic from Cape Verde to Newfoundland between August 20 and September 1. The first storm of the season was a tropical storm that developed in the Gulf of Mexico on July 9 and made landfall along the US Gulf coast before dissipating over Tennessee. ![]() The second hurricane of the season, was the most intense, with maximum sustained winds up to 100 mph (170 km/h). Only two of the systems directly impacted land. Four storms attained hurricane status, with winds of 75 mph (119 km/h) or greater. The Atlantic hurricane database (HURDAT) recognizes five tropical cyclones for the 1872 season.
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