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<br />- - - - - - - - - - - - - - - - - - - <br /> V1 <br /> .j::-- <br />6~ SHADED REGIONS: LWC >0.1 gm/m3 29 DEC 74 <br /> CONTOURS: ICE CRYSTAL CONCENTRATION FLIGHT I <br />5< ... <br /> _______ -230C - - - --- <br /> < <~ < ~;:--"'='I ~~ -...., <br /> . ~- o 0 __ _.........d .d~':- - ,"'" ) \ <br /> ----- --"';, ----- ~ '// / <br /> --------- - -, / <br /> _ 0 @ .;::::;---=----------~o --- / (lOlL) <br /> - 19 C -;;:::;_ - > Olddddddd "dd.. ::-:d . J / / <br /> /,'::':':dd;::'~~ .d. ;; ..) / <br /> / (( (IOO/L) u 0 000'" (50/L) / "- <br /> ;4rl <br /> /\-_ '(l~o/ ......... <br /> / -------- rrRo~ 0_'" '" <br /> ~ ~ "- - )- -'30f ,I' (lOlL) \ GQl (50/L) ~ - ......~ <br /> 1+c ,- <br /> \ <br /> \ <br /> \ <br /> '- --.--------- <br /> 40C -- - <br />2~: - <br />- <br /> ~TARGET AREA---1 <br />- IOKM <br /> I I <br />L <br /> Figure 3.8 Vertical cross section for the first flight of 29 December 1974. Shaded regions show <br /> liquid water contents greater than 0.1 g/m3. Ice crystal concentrations are shown in <br /> parentheses. The diagram is a projection on a vertical plane oriented rrom southwest <br /> (left) to northeast (right). Typical ice crystal trajectories have been added as solid <br /> lines ending on the target area. Each crystal starts as a 10 ~m Pla crystal, and falls <br /> along the trajectory shown as it grows. Considerable variability from these trajectories <br /> is expected in the convective regions. Downwind of the row of stars, seeding would <br /> not produce precipitation on the target area. The trajectory followed by a crystal <br /> railing at a constant 1 mlsec is also shown <br /> <br />