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<br />III. EAGLE RIVER VALLEY-CLIMAX STUDY <br /> <br />The general purpose of the first study was to develop laboratory <br />airflow models which would be adequate in estimating airflow and <br />atmospheric transport-dispersion characteristics during winter storms <br />(northwest winds) over the Eagle River Valley-Climax topographic complex. <br />Both barostromatic and neutral airflow models were investigated because <br />detail information on the meteorological characteristics associated <br />with the winter storms were not established at the outset. <br />The study was different from the other two research efforts in <br />that 1) the topography is principally a long narrow valley, but compli- <br />cated by singular and blocking ridges and 2) the availability of field <br />data made field and model data comparisons more complete than the other <br />two studies. <br />The contents of this section have been condensed from reports <br />submitted by Orgill et ~., (Refs. 30 and 31). <br /> <br />Field Experimental Program <br />The basic features of the Climax weather modification experiment <br />have been discussed by Grant et al., (Ref. 18) and Chappell (Ref. 7). <br />Only information pertinent to~his study will be summarized. <br />1. Network of generators <br />Six silver-iodide ground generators are used in the <br />project. These are Colorado State University modified sky-five, <br />acetone, needle-type ground generators. The seeding rate of the <br />generators may vary from 2 gm/hr to 200 gm/hr of silver-iodide, <br />but are usually set at 15-20 gm/hr which produces about 1014 <br />particles per gm silver-iodide effective at -120C and 4x1015 <br />particles per gm silver-iodide effective at -200C. <br />Two of the six generators are located in the Eagle River <br />Valley which is oriented in 'a northwest-southeast direction from <br />the primary target area (Chalk Mountain). Only northwest wind flow <br />has been used for topographic modeling (Fig. 3-1). <br />The two generators located in the Eagle River Valley were <br />placed near the towns of Minturn and Redcliff. Both generators <br />are deep in the valley but the location of the Minturn generator <br />is upwind from Battle Mountain. <br />2. Criteria for experimental day <br />The decision to turn on the generators during normal <br />operations was made with a randomization scheme. The sampling <br />period was a 24-hour interval of time. <br />The weather criteria used for selecting the experimental <br />days to be used for the prototype studies were: <br />a) deep northwest (270-3600) airflow (5-15 mps) over the <br />area, and <br />b) overcast to broken orographic clouds with some precipitation <br />but of light intensity. <br /> <br />~ <br /> <br />= <br /> <br />G <br /> <br />~ <br /> <br />24 <br />