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<br />Figure <br /> <br />2-1 <br /> <br />3-1 <br /> <br />3-2 <br /> <br />3-3 <br /> <br />3-4 <br /> <br />3-5 <br /> <br />3-6 <br /> <br />3-7 <br /> <br />3-8 <br /> <br />LIST OF FIGURES <br /> <br />Page <br /> <br />"', <br /> <br />Schematic illustr!tion of atmospheric motion <br />and transport-dispersion over irregular terrain <br /> <br />17 <br /> <br />'" <br /> <br />Eagle River Valley-Climax topography and <br />boundaries of topographic model . <br /> <br />Square of the total vector separation R2 <br />versus time. Dual flight #4 in the Camp <br />Hale area . . . . .. .. <br /> <br />25 <br /> <br />29 <br /> <br />Potential and equivalent potential temperature <br />distributions with height at Camp Hale, Colorado. <br />December 12 and 15, 1970 ..... .. <br /> <br />32 <br /> <br />Silver-iodide concentration distribution over <br />three different regions of the Eagle River <br />Valley-Climax area. December 12, 1970 <br /> <br />33 <br /> <br />Silver-iodide concentration distribution over <br />different regions of the Eagle River Val1ey- <br />Climax area. December 15, 1970 . . . . <br /> <br />34 <br /> <br />~ <br /> <br />Silver-iodide concentration distribution over <br />different regions of the Eagle River Val1ey- <br />Climax area. December 15, 1970 . <br /> <br />3' <br /> <br />35 <br /> <br />The approximate horizontal dispersion of <br />silver-iodide seeding material at 13,000 <br />feet m.s.l. as released from Minturn and <br />Redcliff sources. March 12, 1970 ... <br /> <br />36 <br /> <br />Eagle River Valley topographic model during <br />construction and in wind tunnel . . . . . . <br /> <br />37 <br /> <br />3-9 Colorado State University low-speed recircu- <br />lation wind tunnel. .. ..... . . . . . 39 <br /> <br />3-10 Laboratory experimental arrangement for <br />measuring radioactive Krypton-8s concentration ... 41 <br /> <br />3-11 <br /> <br />, 3-12 <br /> <br />Laboratory experimental arrangement for obtaining <br />measurements of the radioactive Krypton-8s <br />concentration over the model for the barostro- <br />matic airflow . . . . . . . . . . . . . . . . . <br /> <br />j. <br />EO <br /> <br />. . 42 <br /> <br />9 <br /> <br />Comparison of selected field potential temperature <br />vertical profiles with a barostromatic model <br />temperature profile . . . . . . . . . . . . . . . . . . 44 <br /> <br />4 <br />