The cold air from the north has to filter through mountain canyons into the basins and valleys to the south. If the cold air is deep enough, it can spill over the mountain ridge. As the air funnels through canyons and over ridges, wind speeds can reach 100 mph, damaging roofs and taking down power and telephone lines. Combining these winds with snow results in a blizzard. In Alaska Wind-driven waves from intense storms crossing the Bering Sea produce coastal flooding and can drive large chunks of sea ice inland, destroying buildings near the shore.
Heavy snow can impact the interior of the state, especially along the southern coast.
The snow accumulates through the winter months and in the mountains, it builds glaciers. The heavy snow accumulations can cause avalanches or collapse roofs of buildings. A quick thaw means certain flooding. Ice jams on rivers can also cause substantial flooding. This Page Printer-Friendly Version BoxerMath Classroom Connect EdGate PH School Scott Foresman SkyLight Professional Development Find a wealth of learning resources for your classroom.