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<br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />001584 <br /> <br />4.6 ELK (Dr. Harold Steinhoff, James Sweeney, John Sweeney) <br /> <br />4.6.1 Job 1. Winter Distribution (James M. Sweeney) <br /> <br />- Objective <br /> <br />To answer the following questions: <br /> <br />1) <br /> <br />What elevations, aspects, and vegetative types <br />are occupied by elk through the winter 8S related <br />to the varying snowpack? <br /> <br />include total precipitation, frequency of storms, and <br />rate of baring of the winter range. The elevation at <br />which elk occur during winter is related to a snow <br />line of a certain critical depth. The location of <br />this critical snow line 1s in turn related to snow- <br />fall patterns during the winter. <br /> <br />Depth of the snowpack at the Top Park fescue study <br />site has proven indicative of winter conditions <br />(Fig. 1). In the first winter of study (1970-71), <br />maximum snow depth (11 decimeters) was not reached <br />until Feb. 27, and decreased from that date on. This <br />could be broadly classified as a mild winter. In the <br />last two winters (1971-72 and 1972-73) a greater <br />depth (14 dm and 16 dm respectively) was reached at <br />an earlier date (Jan. 8 and 6 respectively). The <br />snow was almost this deep already in early December. <br /> <br />The winter of 1971-72 reached a peak on January 8 and <br />decreased from that date on. It could be classed as <br />severe at first, but mild at the end. The last <br />winter, however, should be described as severe <br />throughout. Instead of showing a decrease in snow <br />after January, the snow depth continued to increase <br />until March 31 to a maximum depth of approximately <br />24 dm. <br /> <br />This past winter's flights (15.9 hrs. flight time) <br />over the study area resulted in 465 elk sightings. <br />These sightings indicate that elk began their down <br />slope migration at a time similar to the previous <br />winter of 1971-72 (Fig. 2). By January, however, the <br /> <br /> <br /> <br />1971-72 <br /> <br />~ <br />E 16 <br />" <br />~ <br />I <br />f- <br />a.. <br />W <br />0 <br /> .;- <br />~ .;- <br />e...... <br />0 8 <br />z <br />Vl <br /> <br />2) <br /> <br />What is the critical depth of snow for elk on <br />Missionary Ridge? <br /> <br />FEB <br /> <br />MAR <br /> <br />APR <br /> <br />MAY <br /> <br />- Hypotheses <br /> <br />1) The upper elevationsl limit of elk in winter is <br />dependent upon a critical snow depth, that depth <br />most likely being between 65 and 75 cm. <br /> <br />2) The critical snow depth for elk varies signifi- <br />cantly with abundance of available food, snow <br />hardness, and degree of slope. <br /> <br />3) Elk tend to occur on a south aspect where food is <br />available. <br /> <br />- Findings <br /> <br />E1evation- <br /> <br />Down slope migration patterns of elk in the winter <br />vary with severity of the winter. "Severity" would <br /> <br />24 <br /> <br /> <br />o <br /> <br />NOV <br /> <br />DEe <br /> <br />JAN <br /> <br />Figure 1. Snow depth at The Top Park f~scue study site, Missionary Ridge. <br /> <br />I H <br /> <br />I <br />