• Source: Climate of New York City

According to the Köppen climate classification, the climate of New York City is humid subtropical (Cfa), with parts of the city transitioning into a humid continental climate. (Dfa). The city experiences moderately cold, somewhat wet and snowy winters; and hot, humid summers with plentiful rainfall all year round. As it is more geographically southern, it is usually warmer in winter than in Upstate New York. Also, New York's enormous population, human activity, and vast amounts of large buildings and streets, which absorb sunlight during the day, contribute significantly to the urban heat island effect.
Meteorological records have been kept at Central Park since 1821, although the station was relocated to a different part of the park on January 1, 1920. There are also other weather stations in the area including one at LaGuardia Airport, beginning in 1940, and at JFK Airport, beginning in 1948. However, due to Central Park's long records and central location, it is often considered the main station for the city. Hence, all records unless otherwise stated will be for this station.
The highest temperature ever observed in Central Park is 106 °F (41 °C) on July 9, 1936 - although LaGuardia reported 107 °F (42 °C) on July 3, 1966, and the lowest is −15 °F (−26 °C) on February 9, 1934. The lowest daily maximum is 2 °F (−17 °C) on December 30, 1917. The highest daily minimum at Central Park is 87 °F (31 °C) on July 2, 1903.
The city can be prone to extremes. Snowfall averages 29.8 in (75.7 cm) per year but is highly variable between winter seasons. The city can also be prone to strong winds, being a coastal location it is exposed to the Atlantic. This can be especially pronounced during the autumn and winter months, with a gust of 78 miles per hour (126 km/h) being reported on December 2, 1974. Governors Island, Manhattan, in New York Harbor, is planned to host a US$1 billion research and education center poised to make New York City the global leader in addressing the climate crisis.




Classifications



New York City falls under different climate types depending on the climate classification system used. However, the Köppen climate classification system is the most widely used climate classification scheme, in which New York City falls under the humid subtropical zone.

In the Holdridge life zones system, having a mean annual biotemperature above 53.6 °F (12 °C) and mean annual precipitation above 39.4 inches (1,000 mm), New York City features a warm temperate moist forest climate. By the Trewartha classification, the city is defined as having an oceanic climate (Do). Annually, the city averages 234 days with at least some sunshine. The USDA plant hardiness zones are 7a and 7b. Most of the city is found in 7b, with forested areas and parks being in 7a, as shown in Staten Island and suburban areas. The city also has some small densely populated areas in 8a, like around Laguardia airport.




Temperature


The city's regime of temperature features large seasonal swings, with four distinct seasons. However, due to its proximity to the Atlantic Ocean, these swings are less significant than areas further inland. The Atlantic serves as a moderator of the temperature meaning the city is milder than areas inland during the winter and cooler during the summer. Although, being on the east coast, this effect is less pronounced. All extremes are for the Central Park station.




= Averages

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In an average year, the temperature will usually be between 8 °F (−13 °C) and 97 °F (36 °C) with temperatures greatly exceeding these values being uncommon. Temperatures above 100 °F (38 °C) and below 0 °F (−18 °C) are very rare, with the last occurrences being July 18, 2012 and February 14, 2016, respectively.




= Highest daily temperatures

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= Daily record warm minimum

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= Highest averages

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Precipitation



New York City sees frequent, heavy rainfall. Precipitation averages 49.9 in (1,267 mm) annually. Spring is the wettest season. February is the driest month. Every single month in the city's recorded history has reported some rainfall, showing the variability of the climate. The record for days without rain, is 36 consecutive days, between October 10 and November 13, 1924. The most rainfall in 24 hours was 8.28 in (210.3 mm) on September 23, 1882.
The city sees snow, primarily in winter. It sometimes snows in late autumn and early spring. Snowfall averages 29.8 in (75.7 cm) per year but is highly variable between winter seasons. The most snowfall was 27.3 in (69 cm) on January 23, 2016.




= Averages

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= Rainfall Extremes

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= Snowfall

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Other phenomena






= Sunshine, UV and daylight

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The city generally experiences sunny conditions. As a result of New York City's latitude, 40°42′46″N 74°00′22″W, it is not subject to the extremes of daylight that places much farther north see. However, it is far north enough for there to be a moderate change of possible daylight hours throughout the year.




= Wind

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The wind is seldom strong in New York City but can occasionally be noticeable. This is especially true in the autumn and winter seasons when extratropical depressions often bring strong winds. The strongest gust in Central Park, of 78 miles per hour (126 km/h), occurred on December 2, 1974, however, a station at The Battery reported a gust of 113 miles per hour (182 km/h) on October 14, 1954.
However, tropical storms can sometimes affect the area, although they are infrequent and usually weak. Most recently Hurricane Sandy struck the city on October 29, 2012, causing billions of dollars in damage. It resulted in loss of power, severe flooding and many residents being displaced.




Climate change



Being a coastal city, New York City is expected to experience significant effects from rising sea levels. Predictions that the sea level will rise by as much as 6 feet (1.8 m) by 2100 have prompted the city's mayor to invest $10 billion into keeping the city safe. The city is also expected to become more susceptible to storm surges and flooding, meaning events like Hurricane Sandy's impacts will become more likely in the future.




= Temperature

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The temperature in New York City has generally increased steadily of the last 150 years and this trend is expected to continue due to anthropogenic warming. By 2080, it is predicted that the climate of the city will be similar to northern Arkansas. The mean temperature has risen by 2.4 °F (1.3 °C) since the 1970s and this warming is expected to accelerate in the coming decades.




= Precipitation

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Precipitation in the city has significantly increased since 2000; both rainfall and snowfall have risen, but snowfall has increased much more significantly. However, it is argued that such trends, being so recent, make it impossible to predict whether such increases will continue or become steadier.




Station data



Time series plot for Central Park, 1869–present

See or edit raw graph data.




Notes






References

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