The weather will be mild for most of January, but winter snow will still be falling, which means a lot of winter travelers will be feeling the heat this month.
While the weather will remain warm for most parts of the year, the amount of snow will be much more variable in some places, including parts of Alaska and northern Canada.
The vast majority of snow in January will fall in the northern provinces of Canada, including northern Alberta, Saskatchewan, and northern Manitoba.
Some areas of Canada will get only a little bit of snow, but the majority of winter snowfall will fall as a rainstorm.
While this might seem like a lot, it’s actually less than the amount that falls in any given year.
In the northern states of the United States, only around 20 percent of January snowfall is actually snow.
This number is also quite small compared to the amount the average American receives each year.
For example, in 2017, Americans received around 2.3 inches of snow.
The snowfall for January will be smaller in Canada, which will get about 0.6 inches of the annual snowfall.
Most Canadians receive only a small amount of precipitation.
In January, most Canadians will receive a little over a foot of snowfall in the United Kingdom.
And in April, most of that amount will fall across the United Arab Emirates, while only around a third of it will fall over the Atlantic Ocean.
These statistics come from the US National Snow and Ice Data Center (NSIDC), which monitors global and regional weather and temperature trends for a variety of reasons.
The NSIDC also tracks the snowfall from the surface to the bottom of the atmosphere.
The more snow there is, the higher the temperature.
The lower the temperature, the more precipitation.
This data is also used by NASA to estimate how much snow is left in the global system.
In addition to the actual amount of ice, there are also different types of snow and ice that fall during a winter.
The types of ice are called sea ice and land ice.
While sea ice is composed mostly of water ice, land ice is made up mostly of ice in the ground.
These ice forms over the course of winter, which is why it’s difficult to see exactly how much ice remains.
Sea ice is formed from melting of snow on land, which melts into water ice over time.
When sea ice melts, the water ice inside freezes over.
This freezes and solidifies in the polar vortex.
When this solidifies, the cold air blows over the land, creating the ice.
Sea-ice is the least common type of snow found in the Arctic.
Land ice is a mixture of ice and snow.
It can be either ice, ice-covered snow, or ice-packed snow.
Land-ice can be very large or very small.
As you can see in the map below, the largest land-ice lakes in the world are in Greenland, the Northwest Territories, and Scandinavia.
The largest land ice lakes in North America are in Alaska, the Yukon, and the Northwest Territory.
The size of the land ice in these areas is not as large as in the Antarctic, which has about 100-million-year-old ice.
It’s a good thing for snowpack, because the ice tends to grow in the areas that have more snow.
So when it melts, it produces much more snow than it would otherwise.
In fact, a recent study found that in parts of Western North America, land-mass ice may be more important than sea ice in controlling the amount and quality of winter rain and snowfall because the sea ice acts as a sponge to hold water in.
Land land ice provides about 60 percent of the water in the oceans.
As we’ve mentioned, sea ice provides only about 40 percent of its water.
But in the summer, sea-ice in the lower latitudes will absorb most of the sunlight, and as a result, it will melt more water.
The result is that the ice surface is higher than it is in the winter.
As the water freezes over, it creates more snow and snow, and that snow melts in the same way that water does.
However, this process can also create huge areas of frozen ground.
That ground can become unstable, which can cause roads and bridges to collapse.
This can be especially bad when the road or bridge collapses due to high winds.
But even though the ground freezes over at this point, the snow that falls doesn’t necessarily stop.
As a result of the freezing and the snow melting, there will still have snow on the ground and it will continue to fall.
When the snow melts, some of it falls as rain.
Rain falls in the form of sleet or sleet-like droplets.
This is also the kind of snow that is most difficult to distinguish from rain.
It doesn’t contain any liquid or snow, so the water that falls on the surface is only the snow.
There is another type of precipitation, which happens when the water