New York has a humid continental climate. Weather in New York is heavily influenced by two continental air masses: a warm, humid one from the southwest and a cold, dry one from the northwest. A cool, humid airflow from the North Atlantic also has an effect on weather in the state, albeit to a lesser extent than the continental ones. Many continental frontal boundaries move across New York, and storm systems moving north along the coast often affect the southern areas of the state.
The winters are long and cold in the Plateau Divisions of the state. In the majority of winter seasons, a temperature of −13 °F (−25 °C) or lower can be expected in the northern highlands (Northern Plateau) and 5 °F (−15 °C) or colder in the southwestern and east-central highlands (Southern Plateau). The Adirondack region records from 35 to 45 days with below zero temperatures in normal to severe winters. Much of Upstate New York, particularly Western and Central New York, are typically affected by lake-effect snows. This usually results in high yearly snowfall totals in these regions. Winters are also long and cold in both Western and Central New York, though not as cold as the Adirondack region. The New York City metro area in comparison to the rest of the state is milder in the winter. Thanks in part to geography (its proximity to the Atlantic and being shielded to the north and west by hillier terrain), the New York metro area usually sees far less snow than the rest of the state. Lake-effect snow rarely affects the New York metro area, except for its extreme northwestern suburbs. Winters also tend to be noticeably shorter here than the rest of the state.
New York City has a humid sub-tropical climate. It is the northernmost major city in North America to have this climate.
The rest of New York State has a humid continental climate.
The climate in the New York colony during the 1600-1700s was generally similar to what it is today, with cold winters and warm summers. However, there may have been variations due to natural climate cycles. Overall, the region experienced four distinct seasons with moderate rainfall throughout the year.
New York is generally classified as being in the humid continental climate region due to its four distinct seasons with hot summers and cold winters. However, parts of New York City and Long Island can sometimes experience characteristics of a humid subtropical climate due to urban heat island effects.
In New York State, weather systems like fronts typically move from west to east due to the prevailing westerly winds in the region. Cold fronts generally move faster than warm fronts, which can lead to rapidly changing weather conditions. The movement of these fronts can influence the weather patterns and precipitation in different parts of the state.
In August 2010, New York experienced a typical summer climate with warm temperatures ranging from the 70s to 80s Fahrenheit. It was generally humid with occasional thunderstorms typical of the region during that time of year.
New York experiences a range of extreme weather temperatures. In the winter, temperatures can drop below freezing, especially during cold snaps or polar vortex events. In the summer, temperatures can rise to above 90°F, with heat waves occurring periodically.
New York City has a humid subtropical climate. It is the northernmost U.S. city to have this climate. The rest of New York State has a humid continental climate.
The weather in New York is always changing because it is a temperate climate. This means that New York experiences four distinct seasons throughout the year.
New York City has a humid sub-tropical climate. It is the northernmost major city in North America to have this climate. The rest of New York State has a humid continental climate.
New York City, including Manhattan Island, has a humid sub-tropical climate. The rest of New York State has a humid continental climate.
The climate is the same year-round. The climate for every place on earth is the same year-round. You are confusing climate with weather. See the Related Question below. New York City has a humid sub-tropical climate. The rest of New York State has a humid continental climate. The weather in New York City in the winter is cold, but usually not too cold. Average temperatures in December, January and February range from about 26.9 to 32 degrees Fahrenheit (-2.8 to 0 degrees Celsius). February is the snowiest month, with an average snowfall of 9.4 inches (23.9 cm), followed by January, with an average snowfall of 8 inches (20.3 cm). December is the least-snowy winter month, with an average snowfall of 4.8 inches (12.2 cm). See the Related Link below for more information on New York City's and New York State's climate and weather.
Manhattan is one of the five boroughs of New York City: Manhattan, Brooklyn, Queens, The Bronx and Staten Island. New York City has a humid sub-tropical climate. It is the northermost U.S. city to have this climate. The rest of New York State has a humid continental climate.
I would guess rainy because the rainy weather would move up towards New York state and cause it to rain there.
It can vary greatly throughout the state - remember, New York is a very large state - not just the city. Give a more specific region of New York, and this question can be answered more accurately.
Prevailing north westerlies
New York is the name of the state. The City of New York (New York City) is in the state of New York.
New York is the name of the state. The City of New York (New York City) is in the state of New York.
In 2008, New York State experienced 16 tornadoes according to the National Weather Service data.