- Also called:
- Hurricane Sandy or Post-Tropical Cyclone Sandy
- Date:
- October 19, 2012 - October 29, 2012
Superstorm Sandy
-
What was Superstorm Sandy?
Superstorm Sandy was a massive storm in late October 2012 that caused extensive wind and flooding damage in the Caribbean and the U.S. Mid-Atlantic and Northeastern states. Originating as a tropical wave, it intensified into a Category 2 hurricane before making landfall in New Jersey. The storm merged with a cold air mass, transforming into a sprawling extratropical cyclone.
With a diameter exceeding 900 miles, Superstorm Sandy led to 147 fatalities and caused an estimated $71.4 billion in damages in the United States. The storm surge, amplified by high tides, inundated cities like New York and Atlantic City, disrupting transportation and causing widespread power outages. FEMA's response to Superstorm Sandy was considered a test of reforms implemented after Hurricane Katrina, with emergency declarations signed even before landfall to mobilize assistance.
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When and where did Superstorm Sandy hit the United States?
Superstorm Sandy began as a tropical wave on October 19, 2012, in the central tropical North Atlantic. It progressed westward into the Caribbean Sea and was named Tropical Storm Sandy on October 22 by the National Hurricane Center (NHC).
Sandy reached the U.S. Mid-Atlantic states on October 29, making landfall near Atlantic City, New Jersey, around 8:00 p.m. with sustained winds of 80 miles per hour. The storm caused extensive damage along the coastlines of New Jersey and New York, with a storm surge amplified by high tides due to the full moon on that date.
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What made Superstorm Sandy different from other hurricanes?
Superstorm Sandy was unique due to a combination of factors. A bend in the jet stream, caused by the negative mode of the North Atlantic Oscillation, drew Sandy westward. It merged with a cold air mass, transforming into a massive extratropical cyclone spanning over 900 miles. The storm's westward track over land was also unusual. The storm surge was amplified by high tides due to a full moon. Sandy's impact was widespread, causing damage across 24 states and resulting in approximately $71.4 billion in property damage.
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How did Superstorm Sandy affect people and communities?
Superstorm Sandy had devastating effects on people and communities. The storm caused 147 deaths, with the majority occurring in the Caribbean and the United States. In Haiti, the storm destroyed crops and shelters, leaving approximately 200,000 people without homes.
In the United States, an estimated 8.5 million people lost electrical service. Cities and towns along the Atlantic coast of New Jersey and New York were devastated, and transportation was disrupted with over 20,000 flights canceled. Property damage was extensive, with estimates reaching $71.4 billion by 2014. The Federal Emergency Management Agency (FEMA) reforms were tested, and the response required unprecedented resources and collaboration.
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What kinds of damage did Superstorm Sandy cause?
Superstorm Sandy caused widespread damage across the Caribbean and the U.S. Mid-Atlantic and Northeastern states in late October 2012. The storm's high winds, torrential rains, and coastal storm surges led to 147 deaths and widespread property damage.
Approximately 8.5 million people lost electricity. Cities and towns along the Atlantic coast of New Jersey and New York were devastated. In New York City, a storm surge measuring nearly 14 feet flooded streets and tunnels in Lower Manhattan, and parts of subway lines were inundated. Along the coastline of New Jersey, parts of Atlantic City’s Boardwalk were destroyed, and many homes and businesses were heavily damaged. Overall property damage was estimated at $71.4 billion by 2014.
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How have cities and officials responded to prevent future disasters like Superstorm Sandy?
In response to Superstorm Sandy, which caused extensive damage across 24 states in 2012, various measures were taken to prevent similar future disasters. The reforms that followed Hurricane Katrina were tested, and they were found to have helped create an agency with more foresight and less red tape. President Barack Obama signed emergency declarations for states before the storm made landfall, which helped mobilize assistance and smooth the way for both immediate relief efforts and cash assistance later. A national power restoration task force was created to ensure that all levels of government worked together to restore the energy grid and related infrastructure as quickly as possible.
The Disaster Recovery Reform Act of 2018 was enacted to reduce the cost of future disasters through advance mitigation efforts, such as relocating structures out of flood-prone areas and rebuilding hurricane-proof structures.
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Superstorm Sandy, massive storm that brought significant wind and flooding damage to Jamaica, Cuba, Haiti, the Dominican Republic, The Bahamas, and the U.S. Mid-Atlantic and Northeastern states in late October 2012. Flash flooding generated by the storm’s relentless rainfall, high winds, and coastal storm surges killed 147 people and produced widespread property damage in the areas in its path. The storm swept through the Caribbean as a tropical cyclone (hurricane), and, upon reaching the waters off the coast of New Jersey, it merged with a fast southeastward-moving cold air mass, which drew it westward over land. At its greatest extent, the storm measured more than 900 miles (about 1,450 km) in diameter. The storm caused more than $70 billion in damage in the United States and was among the most costly natural disasters in U.S. history.
Origin and development of the hurricane
Hurricane Sandy began as a tropical wave (a trough of low pressure) in the warm ocean waters of the central part of the tropical North Atlantic on October 19. The system traveled westward into the Caribbean Sea during the next few days, and it was classified as a tropical depression on October 22 in the waters south of Jamaica by the National Hurricane Center (NHC) in Miami. Absorbing energy as it moved northward, the depression grew into a tropical storm, and the NHC named the system Sandy.
On October 24, with sustained 80-mile- (about 130-km-) per-hour winds, Sandy became a category 1 hurricane in the waters just south of Jamaica. After its maximum sustained winds increased to more than 90 miles (144 km) per hour during the late evening, NHC officials reclassified the storm as a category 2 hurricane. Shortly after midnight on October 25, Sandy’s winds rose to 110 miles (177 km) per hour, and by dawn the eye had passed over eastern Jamaica and eastern Cuba.
Between October 25 and October 28, Sandy continued northward but declined in intensity, and it was reclassified as a category 1 hurricane and later as a tropical storm; after passing over The Bahamas and paralleling the coastline of the southeastern United States, the storm had again grown into a category 1 hurricane. On October 29 the storm curved westward toward the Mid-Atlantic states, and by 8:00 pm it made landfall near Atlantic City, New Jersey, with maximum sustained winds of 80 miles (about 129 km) per hour.
Origin and development of the superstorm
Sandy was drawn westward by an unusual bend in the jet stream caused by the negative mode of the North Atlantic Oscillation (NAO). When the NAO is in its positive mode, tropical cyclones and their remnants are caught up in the predominantly eastward flow of the jet stream and quickly thrust out over the cold water of the North Atlantic, where they dissipate. In the NAO’s negative mode, however, the jet stream bends northward over eastern North America. This change results from the presence of a strong high-pressure cell, called a blocking high, that stagnates over Greenland, and any eastward movement of storms behind the blocking high slows substantially.
As the cold air mass—whose leading edge contained a small low-pressure center—approached the hurricane’s warmer counterclockwise wind field on October 29th, winds circulating around the low-pressure centers of the cold air mass and of Hurricane Sandy began to mix. This interaction pulled part of the cold air mass to the south of the hurricane and turned the jet steam separating the two systems westward, which subsequently drew Hurricane Sandy sharply toward the New Jersey coast. Later that day, after the cold air had wrapped around and mixed with the warm air of the hurricane, both systems merged. This development effectively transformed the hurricane into a sprawling extratropical cyclone, which was renamed Post-Tropical Cyclone Sandy by the NHC but was referred to as Superstorm Sandy by meteorologists and newscasters.
Damage
By early 2013, the official number of deaths from Hurricane Sandy, and its later evolution into Superstorm Sandy, was 147, with 72 reported in the Caribbean region, 72 in the continental United States, 2 deaths at sea in the Atlantic, and 1 death in Canada. In the Caribbean, Hurricane Sandy was responsible for approximately 54 deaths in Haiti, 11 deaths in Cuba, 3 deaths in the Dominican Republic, 2 deaths in The Bahamas and 1 death each in Jamaica and Puerto Rico. The high winds and torrential rains that buffeted parts of southern Haiti also destroyed crops and blew away or washed away thousands of tents and temporary structures that were being used to house refugees from the Haiti earthquake of 2010. The hurricane left an estimated 200,000 people without shelter.
However, the bulk of storm-related deaths, injuries, and property damage occurred in the United States. An estimated 8.5 million people lost electrical service as a result of the storm. Several cities and towns along the Atlantic coast of New Jersey and New York were devastated, and the storm surge was made worse by high tides amplified by the full moon that occurred on October 29. Air, rail, and road transportation ground to a halt, with more than 20,000 flights canceled. In the immediate aftermath of the storm, property damage was estimated at between $30 billion and $50 billion; however, this estimate had grown to $71.4 billion by 2014.
In New York City a storm surge measuring nearly 14 feet (about 4.3 meters) combined with heavy rains to cause the Hudson River, New York Harbor, and the East River to flood the streets and tunnels of Lower Manhattan. Parts of subway lines were inundated along with the Hugh L. Carey Tunnel and the Queens-Midtown Tunnel. Flooding and power outages nearby forced the closure of the New York Stock Exchange, the longest weather-related closure of the exchange since 1888.
Along the coastline of New Jersey, damage was extensive. Part of Atlantic City’s world-famous Boardwalk was destroyed, and many of the city’s homes and businesses that were not protected by seawalls were also heavily damaged or destroyed by the storm surge. The boardwalks of Seaside Heights and Belmar were also destroyed, along with many coastal developments along New Jersey’s shoreline. During the storm, water from the Hudson River overtopped the seawall protecting Hoboken and flooded much of the city, isolating an estimated 20,000 residents in their homes.
The effects of Superstorm Sandy were felt throughout the Northeast and the Mid-Atlantic states. Rainfall records were broken throughout the affected area, and roughly 3 feet (about 1 meter) of snow fell in mountainous parts of West Virginia, eastern Tennessee, and western Maryland. Wind and rain disrupted electricity service from parts of Quebec to North Carolina and as far west as Indiana and Illinois.




