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Troendle/Nankervis/Porth Page 17 5/22/2003 <br />Impacts of 2002 fire and insect and disease mortaGty on stream flow <br />The year 2002 was particularly dry and one of the worst fire seasons in recent history. In addition <br />to the catastrophic losses due to fire, mortality associated with insect and disease attack was also <br />perceived to be elevated. As a separate exercise, the Forests provided additional data on the <br />occurrence of fire and insect and disease (pest) mortality in the North Platte Basin for year 2002. <br />Fire data consisted of the defmition of the fire boundary, and identification of the unburned, <br />lightly burned, moderately burned, and severely burned azeas within the fire boundary. Along <br />with providing a GIS layer depicting the area of burn, the Forests also provided a description of <br />the percentage of pre fire basal area remaining after the fire, as a function of specie composition <br />and fire intensity. In addition to the fire data, GIS coverage of aerial surveys for "red tops" or <br />pest kills, in 2002, was also provided. The aerial extent of the pest incidents was much broader <br />than the eactent of fue but the tree mortality was faz less. The pest data consisted of the spatial <br />definition of the polygon surveyed and numbers of red tops, by suspected pest. Although the area <br />of the polygon was defined, along with the number of dead trees, the total number of trees was <br />not listed so a percent reduction in basal azea could not be calculated. In most cases, only a few <br />trees in the polygons were killed and simple calculations indicated that less than 10 percent of <br />the basal area was impacted, at both the polygon and watershed level. A 10 percent or less <br />removal of basal area will not result in a simulated change in stream flow so the impact of pest <br />mortality was dropped from further consideration, hydrologically. <br />Data for three fires, presumed to have occurred on the North Platte basin was provided. As was <br />done with the "activity" data, the first step was to intersect the fire layer with the watershed <br />boundary layer. One of the fires did not occur in the North Platte basin and was dropped. In total, <br />3311 acres of forestland were burned in 2002 in the North Platte basin. This consisted of 1283 <br />acres of spruce-fir, 1414 acres of Ponderosa Pine, 431 acres of Lodgepole Pine, 129 acres of <br />Limber Pine, and 54 acres of Aspen. Most of the area burned was of low to moderate severity <br />meaning that 50 to 80 percent of the initial basal azea survived the fire. The burned azea layer <br />was intersected with the original stand description data layer and the specie composition, initial <br />stand basal azea, reduction in basal azea resulting from fire, and polygon precipitation and aspect <br />deternuned for each separate polygon. T'he SAS model was then run to estimate the impact of <br />fire on water yield. <br />We simulated that the fues that occurred in the North Platte basin in 2002 may have caused the <br />1997 estimate of stream flow of 10.0 inches to increase by 0.01 area inches or 922 acre feet of <br />water per yea.r. This compazes with the estimate of annual increases due to timber harvest <br />activity of about 0.003 azea inches per year. The increase due to timber harvest is accumulative <br />and by 2017 would accrue to 0.05 area inches per year as noted above while the fires of 2002 <br />would be contributing a constant 0.01 area inch. <br />Summary of the Effect of Vegetation Change on Water Yield <br />The most significant factor influencing stream flow from National Forest land in the North Platte <br />River is the amount of precipitation entering the basin on an annual basis. The most significant <br />factor influencing the long-term trends in streamflow response in the basin appears to be the <br />influence of natural changes in vegetation. Forest management activities aze currently having