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<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 />T.rl T~ U WI . " "',.., CllPl: T. au. P!lI; '10 <br /> <br /> <br />.. <br /> <br /> <br />"> <br /> <br />/ <br /> <br />.. <br /> <br /> ", , , '~-r->>(" - <br />\, , \ <br /> \ \, , <br /> \ \ \ \ <br />\, ~-- , , \r <br />',1Ih; "-. >(" V <br /> '" , ,\ . <br /> \ F \ <br /> \. \ V :, \ <br /> \ , <br /> <br />/ , -.< \. \ <br />, ". 'I \. I <br />.. ., ,,,( . '" "/././~' .' , J:, .. ., , <br />.. , .\.. r; <br />'\, . . \ \ \ \ <br />,\ ~.' <br />..,L. -....7-~,..:.... ~ :...:L -~~-i7"-4~- <br />\ /\ . . ? <br />~.>-N<------,-.':-_ .~ - -.....~\,i'\ 1,,' I'_*-"":""""7 <br />t..S/.;7--- / _ . "\6 '\ i.'y-l . I <., ," <br />__ ./ .,'~\ ....' i\ v{ iF <br />,i;-. ,r ~ -"!~\. V-\ ,\_....~~~'l1./' .~, <br /> <br />, <br /> <br />9<'E..T/~-P lAUD 12X111lC 121:mnoo3 ~J1 <br /> <br />La'. "'.11. '-. _1".~ <br /> <br />Figure 2.4 Upper-air soundin2 (taken b)-' a weather balloon) at Grand Junclion, <br />CO at 0500 I\1ST on the mornin~ of Decemher 30~ 2003. The red solid line represents <br />temperature. and the green solid line is the dcwpoint. Blue lines are pressure levels in <br />millibars (horizontal) and temperature in degrees C (diagonal). Red and green dotted <br />lines represent nomlal temperature lapse rates (i.e., change with height). Wind barbs on <br />the right show wind speed and direction at various levels. This panicular sounding <br />shows a temperature of about -10 degrees C al the 700-mb level, which is a good <br />temperature for cloud seeding. However, the lower atmosphere is rather stable in this <br />sounding, making cloud seeding practical only at select locations. <br /> <br />9 <br />