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The Appalachian temperate rainforest has a cool and mild climate and meets the criteria of temperate rainforests identified by Alaback. [1] Temperature and precipitation are extremely variable with elevation, with rainforest conditions usually but not always concentrated around spruce–fir forests at higher elevations.
As Pangea rifted apart a new passive tectonic margin was born, and the forces that created the Appalachian, Ouachita, and Marathon Mountains were stilled. Weathering and erosion prevailed, and the mountains began to wear away. [10] By the end of the Mesozoic, the Appalachian Mountains had been eroded to an almost-flat plain. [10]
In winter, North Carolina is somewhat protected by the Appalachian Mountains to the west. Cold fronts from Canada are typically reduced in intensity by the mountains. However, occasionally cold air can move from the north or northeast, east of the Appalachian Mountains, from Arctic high pressure systems that settle over the Northeastern or New ...
The Uwharries are North Carolina's easternmost mountain range; they are the lowest mountain range in the state. The Uwharries begin in Montgomery County, North Carolina and terminate in the hills of Person County, North Carolina. The highest point in the Uwharries is High Rock Mountain, which is only 1,119 feet (341.1 m) above sea level.
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]
The weather service's outlook for Dec. 8 through Dec. 14 shoes temperatures returning to normal for December for a break from the frigid early December temperatures we will see.
Appalachia (locally / ˌ æ p ə ˈ l æ tʃ ə /, also /-l eɪ tʃ ə,-l eɪ ʃ ə / [4]) is a geographic region located in the central and southern sections of the Appalachian Mountains in the eastern United States.
The state's average annual temperature is 64 °F (18 °C). Temperatures tend to be warmer in the state's southern portion with its proximity to the Gulf of Mexico, while its northern portions, especially in the Appalachian Mountains in the northeast, tend to be slightly cooler. [2]