Typical Weather Pattern for Lake-Effect Snowstorms
C:\Documents and Settings\Bob\Desktop\Work\Book-Edition 3\E3 Chapter 13 Lake Effect Storms\Chapter 13 Final Figures\CH13 Gifs with copyright\Fig.13.02.jpg
qVery cold air must move across a lake surface for lake-effect snowstorms to develop.
qThe warmer the lake temperature and the colder the air, the more extreme the lake-effect  snows will be.
qThis temperature contrast happens most often between late November and mid-January.
qTypically, lake-effect snow begins after an extratropical cyclone has passed over the region and the cyclone’s cold front is well east of the Great Lakes.
qThe strength of this flow is enhanced if an arctic high has moved into the central US.
qUnder these conditions, strong pressure gradient develops across the lakes and drive cold air southeastward from Canada to produce the lake-effect snowstorms.
Snow belts