Tw. Schmidlin et Ra. Roethlisberger, WINTER SUB-FREEZING PERIODS AND SIGNIFICANT THAWS IN THE BOREAL FOREST REGION OF CENTRAL NORTH-AMERICA, Arctic, 46(4), 1993, pp. 359-364
Winter daily maximum temperatures were examined for 56 sites in northe
rn portions of Ontario, Michigan, Wisconsin, and Minnesota over the pe
riod 1960-88. The longest sub-freezing period of winter averaged 20-30
days in the southern portion of the region, 30-40 days around Lake Su
perior, and 90-100 days in extreme northwestern Ontario. These are twi
ce as long as sub-freezing periods at similar latitudes in eastern Can
ada. The sub-freezing period is shortened by about one week along the
shores of the Great Lakes. There is annual spatial correlation of the
longest sub-freezing period, indicating regional synoptic-scale contro
l. The late 1970s had the longest sub-freezing periods but no signific
ant linear trend was found in lengths of sub-freezing periods. The ave
rage date of the first significant thaw (> 10-degrees-C) ranged from e
arly March in the south to late April in the north and is delayed 1-2
weeks along the shores of the Great Lakes.