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Last modified
7/28/2009 2:37:39 PM
Creation date
4/16/2008 11:05:22 AM
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Weather Modification
Title
WMO Training Workshop on Weather Modification for Meteorologists - Lecture Notes
Date
12/1/1979
Weather Modification - Doc Type
Report
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<br /> <br />F-igllfte 9. Spin-06b 06 laftge cilwpJ.> <br />wLth diameteM 06 1.5 - <br />2 mm 6ftom 9 yfta:ting gftowing ha..,U- <br />J.>tcne modelJ.>, J.>pin 6ftequenc.y <br />bft = 3. 17 Hz, YU.Lta:tion-pftec.~J.>ion <br />bftequenc.y 6g = 16 Hz aftound ho~- <br />zontal aUf.> 0 b J.> ymme:tJz.y, M <br />obJ.>eA.ved in the veJt:t.,lc.al meaJ.>u!ting <br />J.>ec.tion at a windJ.>peed 06 31 m6-1, <br />a tempvr.a:twte 06 -100C, an aift <br />pft~J.>llfte 06 50.5 kPa and a liquid <br />wa:teft c.ontent 06 5.1 x ,QO-2 kgm-3. <br />H~:J.>tone diameteft ~ 3 em. <br /> <br />~......... .. <br /> <br /> <br />.', <br /> <br />.... I <br />TIME = 22.' .. <br /> <br />__ - or- - - -:i! ill-."-] <br /> <br />--~._--_...-.- <br />-.-......... .- <br /> <br />1 <br /> <br /> <br />"" <br /> <br />" <br /><". '. <br /> <br />..) \ <br /> <br />2 \,'. _, _.......J <br /> <br />I <br />./ <br /> <br />" <br /> <br />, <br />l' ..'....._ _." <br /> <br />_/ <br /> <br />.. -... - ...... - - - ~ -. <br /> <br />, <br /> <br />--..- <br /> <br />00 <br /> <br />IlK.' <br /> <br />x (K-) <br /> <br />F-igufte 10. ContoWu. 06 doud wa:teft <br />mixing fta:tio and J.>:tfteam- <br />6unction in a :two-dimenJ.,~onal c.loud <br />model a;t :tim~ 22. 8 min and 28.1 mivt. <br />ContOUfl. inteftval 0.5 9 kg -1; aMeft <br />Claftk, 1973. <br /> <br />- 25 - <br /> <br />different parts of a cloud (Figure 11), both <br />according to Clark, 1973. 2-D models, how- <br />ever, have one defficiency, they represent <br />either clouds with slab or cylindrical <br />symmetry and leave no space for the complex- <br />ity in directions of air currents in clouds. <br />3-D models (Klemp and Wilhelmson, 1978; <br />Cotton and Tripoli, 1978) are much better in <br />that respect. The modeller realizes very <br />soon that the evolution of a cloud is con- <br />trolled by the boundary conditions and their <br />variation with time. Thus, for verification <br />purposes, extensive measurement programs in <br />nature are required to know how the boundary <br />conditions could be varied and what the end <br />product would be. <br /> <br />Further, it needs to be said that <br />the computational resources are enormous to <br />deal with the complexities of a single cloud. <br />An example: If one would start to worry in <br />one cloud about the growth of CCN to droplets <br />and the droplet collision problem then the <br />lower end of the space scale would be at lO-6 <br />cm and that of the time scale at 10-7 seconds. <br /> <br />In all objectivity, however, it has <br />to be said that cloud dynamics and numerical <br />modelling has changed Cloud Physics drasti- <br />cally and has brought awareness of many <br />mechanisms and interactions which are so <br />important to the formation of precipitation. <br /> <br />7. Weather Modification Concepts <br /> <br />". <br /> <br />Historically weather modification <br />may have started by fighting the demons <br />behind the severe thunderstorms (the Hittite <br />in Asia Minor used bows and arrows about <br />1400 B.C. according to Pausanias). Later the <br />intent was to blow up or disperse hail clouds <br />by mortars (Leonardo da Vinci) or guns, a <br />method which was practiced up to 1930 in <br />regions near the alpes. In the mid thirties <br />the Swiss engineer named Zimmermann was using, <br />in the good tradition of William Tell, a <br />crossbow to shoot dynamite charges into <br />thunderstorms from an open cockpit aircraft. <br />With the development of war technology, the <br />shock delivery system shifted to rockets with <br />explosive charges. The results were never <br />such that any of those efforts were extended <br />over a sufficiently long period of time to <br />the satisfaction of the consumers. <br />
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