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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). [1] The city experiences moderately cold, somewhat wet and snowy winters; and hot, humid summers with plentiful rainfall all year round.
The climate of New York (state) is generally humid continental, while the extreme southeastern portion of the state (New York City and Long Island area) lies in the warmer humid subtropical climate zone. Winter temperatures average below freezing during January and February in much of the state of New York, but several degrees above freezing ...
The climate of New York City shapes the environment with its cool, wet winters and hot, humid summers with plentiful rainfall all year round. As of 2020, New York City held 44,509 acres of urban tree canopy with 24% of its land covered in trees. [1][2] As of 2020, the population of New York City numbered 8.8 million human beings.
A map of the United States detailing the record-low temperatures for various cities on January 21, 1985. The 1985 North America cold wave [1] was a meteorological event which occurred in January, 1985, as a result of the shifting of the polar vortex farther south than is normally seen. [1]
January 2023 was the warmest on record for multiple cities across the Northeast, including New York City which saw an average temperature of 43.5 degrees Fahrenheit. "That's a whopping 9.8 degrees ...
In New York City temperatures fell to a record low of 4 °F (−16 °C) on January 7, which broke a 116-year record for daily record low. The cold came after days of unseasonably warm temperatures, with daytime highs dropping by as much as 50 °F (28 °C) overnight, as highs were 55 °F (13 °C) early on January 6.
The United States Environmental Protection Agency has noted that "[m]ost of the state has warmed one to three degrees (F) (0.5 - 2 °C) in the last century", [5] and New York State Department of Environmental Conservation has further observed that "[t]he annual average temperature statewide has risen about 2.4 °F (1.3 °C) since 1970, with winter warming exceeding 4.4 °F" (2.4 °C).
The Appalachian Mountains largely shield New York City and Philadelphia from picking up any lake-effect snow, though ocean-effect snows are possible near Cape Cod. [64] The Finger Lakes of New York are long enough for lake-effect precipitation. Lake-effect snow from the Finger Lakes occurs in upstate New York until those lakes freeze over. [65]
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