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Under the Köppen atmosphere characterization, utilizing the 0 °C (32 °F) isotherm, New York City includes a damp subtropical atmosphere (Cfa), and is along these lines the northernmost real city on the North American mainland with this categorization.[204][205] suburbia to the prompt north and west lie in the transitional zone between muggy subtropical and sticky mainland atmospheres (Dfa).[204][205] Annually, the city midpoints 234 days with at any rate some sunshine.[206] The city lies in the USDA 7b plant solidness zone.[207]

Winters are chilly and sodden, and winning breeze designs that blow seaward temper the directing impacts of the Atlantic Ocean; yet the Atlantic and the incomplete protecting from colder air by the Appalachians keep the city hotter in the winter than inland North American urban areas at comparable or lesser scopes, for example, Pittsburgh, Cincinnati, and Indianapolis. The day by day mean temperature in January, the territory's coldest month, is 32.6 °F (0.3 °C);[208] temperatures as a rule drop to 10 °F (−12 °C) a few times for each winter,[209] and achieve 60 °F (16 °C) a few days in the coldest winter month. Spring and pre-winter are capricious and can run from nippy to warm, despite the fact that they are generally mellow with low stickiness. Summers are regularly warm to sweltering and moist, with an every day mean temperature of 76.5 °F (24.7 °C) in July.[208] Nighttime conditions are frequently exacerbated by the urban warmth island marvel, while daytime temperatures surpass 90 °F (32 °C) by and large of 17 days each mid year and in a few years surpass 100 °F (38 °C). Extraordinary temperatures have extended from −15 °F (−26 °C), recorded on February 9, 1934, up to 106 °F (41 °C) on July 9, 1936.[208] The normal water temperature of the close-by Atlantic Ocean ranges from 39.7 °F (4.3 °C) in February to 74.1 °F (23.4 °C) in August.[210]

The city gets 49.9 inches (1,270 mm) of precipitation every year, or, in other words spread consistently. Normal winter snowfall somewhere in the range of 1981 and 2010 has been 25.8 inches (66 cm); this fluctuates impressively between years. Sea tempests and typhoons are uncommon in the New York area.[211] Hurricane Sandy brought a ruinous tempest flood to New York City on the night of October 29, 2012, flooding various boulevards, passages, and tram lines in Lower Manhattan and different zones of the city and cutting off power in numerous parts of the city and its suburbs.[212] The tempest and its significant effects have incited the discourse of building seawalls and other beach front obstructions around the shorelines of the city and the metropolitan territory to limit the danger of dangerous outcomes from another such occasion later on.

The City of New York has a mind boggling park framework, with different terrains worked by the National Park Service, the New York State Office of Parks, Recreation and Historic Preservation, and the New York City Department of Parks and Recreation.

In its 2013 ParkScore positioning, The Trust for Public Land detailed that the recreation center framework in New York City was the second best stop framework among the 50 most crowded US urban areas, behind the recreation center arrangement of Minneapolis.[218] ParkScore positions urban stop frameworks by an equation that investigates middle stop measure, stop sections of land as percent of city zone, the percent of city occupants inside a half-mile of a recreation center, spending of stop administrations per inhabitant, and the quantity of play areas per 10,000 inhabitants.



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