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The annual average temperature across the state ranges from around 39 °F (4 °C) over the Adirondack Mountains to near 53 °F (12 °C) across the Hudson Valley and Long Island, to around 56 °F (13 °C) within New York City. [2] Weather in New York is heavily influenced by two air masses: a warm, humid one from the southwest and a cold, dry ...
The list of snowiest places in the United States by state shows average annual snowfall totals for the period from mid-1985 to mid-2015. Only places in the official climate database of the National Weather Service, a service of NOAA, are included in this list. Some ski resorts and unofficial weather stations report higher amounts of snowfall ...
The Tug Hill town of Montague in Lewis County recorded the unofficial New York State 24-hour snowfall record of 77 inches (6.4 ft; 2.0 m) in January 1997. [5] Hooker (a hamlet in the town of Montague) holds the state record for snowfall in a single season, after accumulating 466.9 inches (38.91 ft; 11.86 m) of snow during the winter of 1976–1977.
A 60-mile stretch of the New York State thruway, closed Saturday, was open Sunday but banned commercial vehicles. Here's a look at some of the astounding snow totals in northern New York state.
Pounding snow and bitter cold continued their assault across the nation's northern tier Monday after dumping five feet of snow in some areas of New York state and three feet or more in parts of ...
The snow was not as heavy in downtown Philadelphia, where around 2 inches was measured, although more than half a foot was reported in suburbs north and ... 3.2 inches fell in New York City, the ...
The climatic snow line is the boundary between a snow-covered and snow-free surface. The actual snow line may adjust seasonally, and be either significantly higher in elevation, or lower. The permanent snow line is the level above which snow will lie all year.
Snow accumulation on ground and in tree branches in Germany Snow blowing across a highway in Canada Spring snow on a mountain in France. Classifications of snow describe and categorize the attributes of snow-generating weather events, including the individual crystals both in the air and on the ground, and the deposited snow pack as it changes over time.