There's probably snow in the mountains of northern Georgia.
56.1" as of Jan 28 2011
In the far north where the terrain is ice and snow.
76.5" as of Jan 27 2011
Yes, but it all depends on where the grassland is located (the elevation or how far north/south it is). The higher the elevation and the closer the grassland is to the North or South Pole, the more likely it is to get snow.
Canada is far up in the north where the climate is very cold, so it tends to get more snow than other places.
There is only about five percent humidity in Antarctica. Sometimes it does rain in the far north end of the Antarctic peninsula. 'Snow' is really blowing ice crystals and not snow at all.
Cincinnati had received 21.8" of snow as of the climate report at 12:37am Jan 12, 2010 (and currently snowing). This compares to the average for this point in the winter of 7.6".
Impossible to say, but probably not, it's too far south to get any real snow. Move North.
In the mountains and far north receive 100 or more inches annually.
It snows more in northen states because those states are far away from the equator. The equator is the hotest part of the world So where it's far down south or far up north there's ice. Examples: Antarctica is far down south with ice and Greenland is far up north with ice.
It is very unlikely for lake effect snow to reach North Carolina. Lake effect snow is typically associated with the Great Lakes region of the United States, where cold air passing over the relatively warm waters of the lakes picks up moisture and creates heavy snowfall. North Carolina's climate and geography make it rare for lake effect snow to reach that far south.
In the far north, the far south, and on mountain tops, it gets cold. It snows. In some places, it takes a long time for the snow to melt. Sometimes the snow does not melt during the summer. Instead, the snow stays there and the next years snow lands on top of the old snow. This creates a snow field. As time goes by, the snow field becomes more and more compressed. The snow field turns to ice. It turns into an ice field. Then, the ice field begins to flow in one or more directions. At that point it became a glacier.