Laserfiche WebLink
<br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br /> <br />years duration (20 years or more if possible). These records are partitioned into those located <br />within the designated "target" area ofthe project and those in a nearby "control" area. Ideally the <br />control sites should be selected in an area meteorologically similar area to the target, but one <br />which would be unaffected by the seeding (or seeding from other adjacent projects). The <br />historical data (e.g., precipitation) in both the target and control areas are taken from past years <br />that have not been subject to cloud seeding activities. These data are evaluated for the same <br />seasonal period of time as that when the seeding later was conducted. The target and control sets <br />of data for the unseeded seasons are used to develop an equation (typically a linear regression) <br />which predicts the amount of target area precipitation, based on precipitation observed in the <br />control area. This regression equation is then used during the seeded period, to estimate what the <br />target area precipitation should have been without seeding, based on that observed in the control <br />area. This allows a comparison to be made between the predicted target area precipitation and <br />that which actually occurred during the seeded period, to look for any differences potentially <br />caused by seeding activity. <br /> <br />This target and control technique works well where a good historical correlation can be <br />found between target and control area precipitation. Generally, the closer the target and control <br />areas are geographically, and in terms of elevation, the higher the correlation will be. Areas <br />selected too close together, however, can be subject to contamination of the control area by the <br />seeding activities. This can result in an underestimate of the seeding effect. For precipitation and <br />snowpack assessments, a correlation coefficient (r) of 0.90 or better would be considered <br />excellent. A correlation coefficient of 0.90 would indicate that over 80 percent of the variance <br />(r2) in the historical data set would be explained by the regression equation used to predict the <br />variable (expected precipitation or snowpack) in the seeded years. An equation indicating <br />perfect correlation would have an r value of 1.0. <br /> <br />In this particular case, one potential target site (McClure Pass, which measures data <br />appropriate for both the precipitation and snowpack evaluations) was considered questionable <br />due to its location near the northern boundary of the target area, where lesser seeding effects <br />might be expected to occur due to targeting considerations. Also, there was the question of <br />potential contamination due to its proximity to another historical seeding program over the <br /> <br />45 <br />