What is the Hazard?

Coastal storms happen when different meteorological conditions converge. Coastal storms are organized systems that have unique characteristics, but each type can turn deadly due to their hazardous consequences — sustained destructive winds, heavy rainfall, storm surge, coastal flooding, and erosion.

New York City experiences hazards from two types of coastal storm systems:

Storm Types

Tropical cyclones are organized systems of thunderstorms that form over warm tropical ocean waters. These systems rotate counterclockwise in the northern hemisphere around a low-pressure center and are classified into three types:

  • A tropical depression is an organized system of clouds and thunderstorms with a defined surface circulation and maximum sustained winds of 38 miles per hour (mph) or less.
  • A tropical storm is an organized system of strong thunderstorms with a defined surface circulation and maximum sustained winds of 39 to 73 mph.
  • A hurricane is an intense tropical weather system of strong thunderstorms with a well-defined low-pressure center (“eye”) and maximum sustained winds of 74 mph or greater.

Several conditions must be in place for tropical cyclones to form and maintain their intensity. Most importantly, as a general rule, water temperatures must be greater than 80°F in the present climate. Tropical cyclones that affect New York City originate in the North Atlantic Basin. Conditions that cause tropical cyclones to form are most likely to occur off the coast of Africa, in the Caribbean Sea, and in the Gulf of Mexico.

Once tropical cyclones form, they often track northward or westward until they reach the mid-latitudes (usually the northern Gulf of Mexico, southeastern United States, or the northwest Atlantic), where they turn northward or eastward in response to the prevailing winds. However, when certain meteorological conditions coincide, they may track up the East Coast of the United States and head toward New York City.

The Atlantic hurricane season is June to November. According to the National Hurricane Center (NHC), the Atlantic hurricane season began showing a pattern of heightened activity in 1995 – a trend that continues through today.

The North Atlantic Basin has an average of 12 tropical storms and six hurricanes per year. New York City is at highest risk between August and October when water temperatures are warmest and meteorological conditions in the North Atlantic Basin favor storm formation.

The hurricane risk to New York City peaks in mid-September. Although water temperatures as far north as New York City rarely reach 80°F around this time of year, waters are sufficiently warm to allow strong hurricanes to sustain high energy as they make landfall in the New York region.

Primary Hazards Associated with Hurricanes

Primary Hazards Associated with Hurricanes

Source: NYCEM

When tropical systems make landfall, the primary hazards are heavy rain, high winds, tornadoes, and storm surge. The most dangerous conditions arise in two specific areas of a hurricane -- near the center of circulation, or eye wall (the region surrounding the eye), and in the right-front quadrant of the storm, where the hurricane’s high-speed forward motion accelerates the impact of high winds and storm surge.

Heavy rain from tropical systems can occur throughout the duration of a storm. As shown in the illustration, the heaviest rain typically falls on the left side of the storm’s eye when it impacts the New York region. The amount of rainfall depends upon the storm’s speed, size, and the geography of the area it traverses, not on its classification.

The hazards from heavy rain are freshwater flooding when rivers and streams overflow their banks, and inland (flash) flooding in low-lying areas if ground or drainage systems lack the capacity to absorb the unusually high rainfall.

The strongest winds from tropical systems typically occur on the storm’s right side. The primary hazards from strong winds are downed trees and power lines, structural damage to buildings and property, and flying debris.

Tornadoes commonly form either in the right-front quadrant of the storm, in the storm’s eye wall, or in thunderstorms embedded in rain bands far from the storm’s center. Tornadoes produced by tropical cyclones are usually weak and short-lived, but have the potential to pose deadly hazards.

Storm surge is the tropical-cyclone hazard responsible for greatest number of deaths, as shown in the graphic.

Storm surge occurs when water level rises abnormally above the typical astronomical tide level. Storm surge happens as the force of the wind and low pressure of the storm push water toward shore. During high tides, the surge causes the mean water level to rise even higher, severely inundating coastal areas. Storm surge is measured by calculating the difference between the normal astronomical tide level and the observed storm water level, or storm tide.

The intensity of the storm surge depends upon several storm characteristics including the maximum sustained winds, forward speed of the storm, size of the wind field, direction of the storm's track at landfall, and the geography of the coastline. The most significant storm surge typically occurs near the eye and in the right-front quadrant of the storm.

The illustration shows how an advancing surge combines with a normal tide to create the hurricane storm tide that can inundate a coast.

Combined Effects of Storm Surge, Tide, and Wave Action

Combined Effects of Storm Surge, Tide, and Wave Action
Storm tide values are always referenced to a vertical datum, typically Mean Lower Low Water (MLLW). MLLW is the average height of the lowest tide (lower of the two daily low tides) recorded daily at a tide station.

Inundation caused by storm surge can be measured by the height (or depth) of water above ground level. This is calculated by measuring the height of the total storm tide and subtracting the local land elevation (referenced to a vertical datum). For example, a storm tide height of 20 feet at a land elevation of five feet results in 15 feet of storm-surge inundation.

Coastlines along the open ocean are exposed to two types of tropical cyclone hazards -- stillwater flooding from storm surge and tides and extremely powerful wave action superimposed upon the storm tide. The hazards resulting from this type of extremely forceful wave action include damage to the beach, local buildings, property, and infrastructure.

A nor'easter is a type of coastal storm that primarily affects the Mid-Atlantic and New England states, between October and April. Like tropical cyclones, nor’easters are associated with heavy precipitation and a counterclockwise rotation around a center of low pressure. The following chart summarizes the differences between tropical cyclones and nor’easters.

Characteristics of Coastal Storms

Tropical Cyclone Nor'easter
  • Forms in tropics or subtropics
  • Forms over water
  • Derives energy from warm ocean water
  • Occurs between June and November
  • Often associated with bands of severe thunderstorms and possibly tornadoes
  • Not associated with wintry precipitation (snow, sleet, freezing rain)
  • Forms outside of the tropics
  • Forms and maintains strength over either land or water
  • Derives energy from temperature contrasts in the atmosphere
  • Occurs between October and April
  • Rarely associated with severe thunderstorms and tornadoes
  • Often associated with wintry precipitation (snow, sleet, freezing rain)

Unlike tropical cyclones, nor'easters form outside of the tropics, typically over the northwestern Atlantic, northern Gulf of Mexico, or central or western United States. Nor’easters can originate and sustain themselves over land and are able to form during the cooler months of the year.

When these storms reach the Northeast or Mid-Atlantic coast, the counterclockwise circulation brings winds from a northeasterly direction—hence the name nor'easters. Although nor'easters are typically weaker than hurricanes, they may be larger and have durations lasting multiple tide cycles, creating the risk of more widespread impact. Nor'easters occur more frequently than hurricanes in the New York City area. Due to their frequency, the risk posed by hazards from nor'easters could be considered cumulatively greater than those from hurricanes.

The hazards posed by nor'easters are heavy precipitation, inland flooding, and winds typically strong enough to knock down trees and power lines, causing widespread disruption and structural damage to buildings. Nor’easters may also create coastal flooding from storm surge and large waves.

The hazards of heavy snowfall, sleet, and freezing rain are often associated with nor’easters (see Winter Storms ). When a wintertime nor'easter moves up the Atlantic coast and follows a track west of New York City, precipitation often changes from snow or sleet to rain. If a nor’easter maintains a track just off the coast of the city, snow or mixed precipitation likely occurs.

Coastal Storm Attributes/Characteristics

The severity of a tropical storm depends on multiple factors.  However, the ferocity of tropical storms is formally categorized on the basis of wind speed as measured by the Saffir-Simpson Hurricane Wind Scale. This scale categorizes a hurricane's intensity on a scale ranging from one to five based on the storm's maximum sustained wind speed. Levels of potential property damage are associated with each of the five categories. Hurricanes categorized 3 or higher are considered major hurricanes. This scale does not indicate the amount of surge or rain expected from a hurricane, only wind.

The illustration below describes the severity categories for tropical storms associated with New York City. Category 4 hurricanes in the New York City region are possible, but unlikely. Category 5 hurricanes are not anticipated to occur in the New York City area, because they are not meteorologically sustainable over the Atlantic Ocean north of Virginia.

Source: National Hurricane Center

Although the Saffir-Simpson Hurricane Wind scale is a practical way of measuring hurricane strength, other factors contribute to a hurricane's impact on a given location -- the storm's size (proportional to the radius of maximum winds) and speed of its forward motion. A larger, slower-moving storm, for example, may cause greater damage than a smaller, faster-moving storm with high winds because a single location might be battered by winds from a slower-moving hurricane for a longer period of time.

The wind’s fetch -- the distance that the wind blows across the water’s surface -- and its duration also affect a tropical cyclone’s severity.  Wind fetch is determined by the radius of maximum winds and forward speed of the tropical storm. The severity of waves and height of the storm surge is directly affected by how far and how long a specific storm’s winds blow across the water.

A Hypothetical Storm Approaching New Jersey

The bearing of a storm —the direction that it is moving — when it reaches New York City also contributes to the severity of its impact.  Its bearing determines the wind direction, which affects the height and severity of the storm surge.

The local geography of the coastline amplifies storm surge in the New York City region. The New York Bight – the nearly 90-degree angle formed by the shorelines for Long Island and New Jersey – can direct a storm surge directly into New York Harbor. Storms with a westward bearing often generate higher storm surge risk.

For New York City, the worst-case hurricane track is a storm making landfall just to the south along the coast of New Jersey. In this scenario shown in the illustration below, the city is in the right-front quadrant of the storm as the storm funnels the surge directly into Raritan Bay and New York Harbor.

This scenario is precisely what happened in 2012 during Hurricane Sandy and why the storm had such a disastrous impact on New York City. Hurricane Irene made landfall over Brooklyn in 2011, but was a very different tropical storm than Sandy. At landfall, Hurricane Irene’s bearing was north-northeast, which did not create the direct surge impacts that Hurricane Sandy inflicted on New York City just over one year later.

Nor'easters do not have a universally recognized classification system, but their strength and severity are influenced by factors similar to those discussed regarding the severity of tropical storms.

When a Nor’easter produces a heavy snowfall, the Northeast Snowfall Impact Scale (NESIS) is used to measure the intensity of wintry precipitation. The NESIS characterizes and ranks high-impact Northeast snowstorms – those with large areas of snowfall accumulations of 10 inches and greater – on a scale of one to five.

The National Climatic Data Center developed this scale to indicate the degree to which Northeast snowstorms might affect the transportation systems and economy of the region and thereby impact the rest of the country. The NESIS index incorporates population data and meteorological measurements to gauge a nor’easter storm's overall impact.

The National Hurricane Center (NHC) forecasts storm tide heights for tropical storms and hurricanes on a probabilistic basis (a range of likely storm tide levels) and updates its forecasts regularly as specific storms approach landfall.

The NHC calculates return periods for hurricanes for various locations along the East Coast of the United States. These return-period calculations represent the average amount of time between the passages of two hurricane eyes within a 50-nautical-mile (57.54-mile) radius of a given location.

According to these NHC probability models, New York City should expect to experience a lower-category hurricane on average once every 19 years and a major hurricane (Category 3 or greater) on average once every 74 years.

The National Oceanic and Atmospheric Administration (NOAA) provides timely storm tide forecasts for non-tropical storms (including nor'easters) on a deterministic basis (a single value for each tide gauge location). New York City typically experiences several nor'easters of different intensity every year. Most of these nor’easters are relatively weak but retain the potential to produce significant rainfall or snowfall hazards that can cause minor-to-moderate damage across the area. The probability of severe nor'easters affecting New York City is low, but they do strike occasionally.

Some academic institutions, including Stevens Institute of Technology and SUNY Stony Brook, provide forecasting services similar to NOAA. Although conducted purely for research purposes, their forecasts are often valuable supplements to official forecasts.

The vulnerability of different neighborhoods and areas of New York City to hazards associated with tropical storms varies significantly. To predict storm surge and to guide the City's planning for coastal storms, New York City Emergency Management (NYCEM) utilizes outputs from a National Hurricane Center computer model called SLOSH (Sea, Lake, and Overland Surges from Hurricanes).

The SLOSH model calculates surge heights for storms that move in different directions and vary in strength from Category 1 to Category 4. Calculations are based on the different wind speeds associated with Category 1-4 storms, the radius of maximum winds, the storm’s forward speeds, storm bearing, and tides. The SLOSH model calculates surge levels for specific locations assuming that each location is hit by the most intense part of a storm. The SLOSH model uses all of these factors to generate a worst-case scenario for storm surge at specific locations in New York City, it does not relate to probability of occurrence.

The map below shows areas of the city likely to experience inundation from different categories of storms, based on the SLOSH model calculations. The extent of inundation and storm-surge depths indicated on the map reflect the worst-case scenario for Category 1-4 hurricanes in different parts of New York City.


An important characteristic of any tropical storm is the amount of coastal flooding it causes. Meteorologists often report on the level of storm surge – that is, the amount of additional water above mean (average) sea level -- that the coastal storm creates.

Reporting storm surge alone does not always represent the amount of coastal flooding created by a storm. If depth of coastal flooding at a specific location needs to be determined, two other factors must be incorporated – the land’s elevation above mean sea level at the location and tide levels at the time of the storm’s landfall. For example, the tide level can range up to eight feet in the New York City area. The difference between storm surge and depth of coastal flooding was a point of confusion among public officials, the media, and the general public during Hurricane Sandy.

The National Hurricane Center developed an experimental Potential Surge Flooding Map to simplify predictions of storm surge flooding. Launched for the 2014 hurricane season, this NHC tool forecasts the potential depth of coastal flooding during a particular storm, incorporates uncertainties, and providing periodic updates as the storm progresses.


The likely inundation depths listed under each location on the map reflect the difference between the height of the storm tide projected for each hurricane category and the land elevation of that specific area in New York City. The red areas on the map represent the areas of the city that could be inundated by storm surge in a worst-case scenario from a Category 1 hurricane.

NYCEM utilized SLOSH data to develop evacuation zones for the New York City Coastal Storm Plan (CSP). Evacuation zones are based on a SLOSH output called Maximum Envelope of Water (MEOW). MEOWs show the maximum surge inundation from a set of hypothetical storms of fixed size at specific landfall locations with varied intensity, forward speed, storm direction, and tide anomaly.

The CSP evacuation zones employ a range of possible scenarios from the MEOWs, in contrast to the SLOSH maps that only display one worst-case scenario storm surge, the MOM (Maximum of MEOWs) for each category.

Evacuation zones presume a universal worst-case scenario, as if a storm were to make landfall in all parts of the city at once, creating the maximum amount of potential surge inundation in each location. Evacuation orders are issued for an entire zone due to the inherent uncertainty in the forecast, even though a storm will not create worst-case effects in every part of the zone.

The City updated its evacuation zones in June 2013. Unlike the prior set of evacuation zones, which were in place when Hurricane Sandy struck in 2012, the storm's bearing is now a more significant input for the calculation of the new zones.

SLOSH data is not used for nor’easters. However, the National Weather Service provides water level forecast ranges referenced to MHHW and MLLW for tidal gauges around the New York City metro region ahead of an impending coastal flood event. Then, NOAA’s Office for Coastal Management Sea Level Rise Viewer and NWS New York Impact Catalogs is used to determine the potential impacts from that storm.

To see records of coastal storms affecting New York City since 1785, use the Hazard History and Consequence Database, an interactive tool developed for this website.

The figure below shows the tracks of coastal storms to come within 100 miles of New York City between 1851 and 2018.

Tropical Storm and Hurricane Tracks within a 100-mile Radius of New York City, 1851 to 2018

Historical Tropical Storm & Hurricane Tracks


Since the 2014 Hazard Mitigation Plan, the City has had at least three close calls with tropical cyclones that were predicted to make landfall in New York City:

  • Tropical Storm Joaquin in October 2015
  • Tropical Storm Hermine in September 2016
  • Hurricane Matthew in October 2016

Even though these forecasted storms did not significantly impact the New York City area, they serve as a reminder of the risk that the City continues to face from coastal storms.