White-tailed deer (Odocoileus virginianus) were marked and followed by telemetry between December 1969 and May 1972 to determine their seasonal home ranges, distribution by forest cover types, and their movements in response to snow depth, precipitation, barometric pressure, temperature, wind, windchill, and time of day. Twenty-eight deer were radioequipped and 22 (12 adults, 5 yearlings, and 5 fawns) were relocated. Sizes of home ranges were measured by computerized movement maps: 949 ha for three deer in a snowfree winter; 88 ha for seven deer ina winter of deep snow, 341 ha for five deer in a winter of average snowfall, and 266 ha for five deer in two summers. In a winter of deep snow, the area used declined to 7.3% and distance travelled per hour to 76% of their respective values in a snowless winter. Windchill, barometric pressure, and temperature had less effect on deer movements as snow accumulated. Deer moved mostly in later afternoon--evening and early morning in winter, and mid-day and evening at other times of the year. Relocations indicated a preference of deer for mixedwood cover throughout the year, but as snow accumulated use of softwood increased. Deer moved to winter ranges when snow accumulated to 30 cm in hardwood stands and returned to summer ranges after several days of temperatures above 5.5C. Some deer moved up to 20 km from summer to winter ranges. Improved interspersion obtained by modifying sylvicultural practices could provide ample winter habitat in areas considerably smaller than the 300-400 ha measured. Areas of 300-400 ha with many small clear-cuts provided adequate summer habitat.
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Charles-A. Drolet (1976) studied this question.
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