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Last modified
7/28/2009 2:40:21 PM
Creation date
4/24/2008 2:48:39 PM
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Weather Modification
Title
Papers Presented at the 17th Annual Canadian Meteorological and Oceanography Congress
Date
5/1/1983
Weather Modification - Doc Type
Report
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<br /> <br />-;: 400 <br />~ c: <br />... Q) <br />0.- <br />Q) ~ <br />Cl '5 300 <br />~ cr <br />o Q) <br />c: Gi <br />~ til 200 <br />I'D ~ <br />Q) E <br />~ .E 100 <br /> <br />500 <br /> <br />.. Cases <br /> <br />,., <br /> <br />~ <br /> : <br />. . <br />,.. <br />;. <br />~ - .... n. n_ .- .- ....-.. ....... I <br /> <br />Jan Feb Mar Apr May 1 May 15 June <br />Date <br /> <br />Figure 7. Average snow water equivalent over the <br />measurement season for 70 Alberta, B.C. and Montana <br />snow courses. <br /> <br />\ ,0 " <br /> <br />~ G ,8 - <br />7- <br />c. <br /> <br />8 <br /> <br />t: 0 .6 - <br /> <br />"'/ <br />U <br /> <br />i.) <br />~ u .~ - <br />.... <br />-l <br /> <br />'., <br /> <br />;;:.. <br />'''; C .2 .- <br /> <br />~--~.--.--' <br /> <br /> <br />;\']~ sa <br /> <br />~'J/ <br /> <br />occ <br /> <br />.110:, <br /> <br />FTIl <br /> <br />,.w~ N'R ,'j,' <br /> <br />u:; <br /> <br />i":O,'JTH" <br /> <br />Figure 9. Seasonal variation of the correlation be- <br />tween average monthly snowfall and station elevation <br />for 57 A.E.S. climate stations. <br /> <br />T <br /> <br />BGll--r <br /> <br />Y . -B3 . 0,33 X <br /> <br />/ <br /> <br />c <br />v?, 0,73 <br /> <br />-' <br /> <br />600 c <br /> <br /> <br />2500 <br /> <br />F' <br />. ~~ <br />o <br />"?: <br />to , <br />..J /,00 " <br />~ <br /> <br />:1 . 57 CLl~,;,T[ STATIC':S <br /> <br />: <br /> <br />t.~ <br /> <br />uJ <br />i:'! 200 - <br />co I <br />~ <br />a: <br /> <br />nl <br />SG~ <br /> <br />, I <br />1000 i5:0 2000 <br />STA-:'IO:ol EL::V":'ION Cm MSL) <br /> <br />, <br /> <br />-\ <br />j <br />I <br /> <br />Figure 8. Variation of average annual snowfall with <br />station elevation for 57 mountain A.E.S. climate sta- <br />tions. The calculated linear regression least squares <br />fit and correlation coefficient are also shown. <br /> <br />-1 <br /> <br />i :' 0 0 <br /> <br />Y..!70'O,32X <br /> <br />" <br /> <br />R . 0,33 <br />R . 0,59 (1IITH3UT ;',:'.:;...:') <br /> <br />lI' e <br /> <br />J:, <br /> <br />t <br />~ 1 000 ~ <br />~ ' <br />~ <br />c:' <br />2: <br /> <br />.. .~ <br />.. :........:~.............., <br /> <br />...---.:-=---- .: ' <br /> <br />. ---/~~ +.. ...* <br />.. ..t;.... ....:. + <br /> <br />. ...~.;,_:...,~~. '. <br />. I , <br />1000 1500 2GOO <br />S~OE: E~E"'ATION Cm MSL) <br /> <br />.. <br /> <br />... <br /> <br />lI' <br /> <br />. . <br /> <br />=> <br />':) <br />uJ <br />~ 500 <br /> <br />~ <br /> <br />$ <br /> <br />. <br /> <br />.. <br /> <br /> <br />o <br />500 <br /> <br /> <br />2500 <br /> <br />Figure 10. Seasonal variation of average snow water <br />equivalent with elevation for 70 Alberta. B.C. and Mon- <br />tana snow courses. Linear regression lines and correla- <br />tion coefficients calculated both with and without the <br />Montana data are also shown. <br /> <br />10 <br />
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