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Last modified
7/28/2009 2:27:42 PM
Creation date
10/1/2006 2:12:32 PM
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Weather Modification
Applicant
Western Weather Consultants
Project Name
Vail Pass
Date
11/1/1984
Weather Modification - Doc Type
Application
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<br />BACKGROUND OF CLOUD SEEDING FOR THE SAN JUA.."'{ ECOLOGY <br />11 <br />PROJECT- (W. Howell. U.S. Bureau of Reclamation) <br />. <br /> <br />When winter snowstorms s~eep over the San.Juan Houn-. <br />tains. not all of the moisture that condenses in the <br />form of clouds above the mountains falls as snow. <br />Much of it remains-in particles too small to fall. <br />Carried beyond the mountains by the wind to where the <br />airflow sinks once more toward the plains. these par- <br />ticles re-evaporate. The rate at which snow reaches <br />.the ground. expressed as a proportion of the rate at <br />which mo1stur~condenses In the cloud~ is called the <br />efficiency of precipitation. . <br /> <br />It has been found that in.some.storms. especially <br />those having relatively deep cloud systems ~lth cloud- <br />top temperatures below about -27 C. the precipitation <br />efficiency tends to be relatively high. and in such <br />situations there i. little that the current knowledge <br />of weatber =odiftc.tion could do to increase the.sno~- <br />falL In weak . tl3ms that .condense very little cots- <br />tu~e. 'there Is l1iltwise little potential for...st1mula-..- <br />tion. Ho~ver:. to: has been found that when t~ ~_._. <br />clouds are-deep eno'l'.h and active enough to Cilr.ct4!'t'JI&SQ <br />r.,;-la:lvely large .l~Ount5 of moisture but the ..:llw::, <br />top temperature is warmer than about -26 c. seedln~ <br />of the clouds witn artificial ice nuclei often raises <br />the prec~p1tatlon etI1c1ency tram a rather low va~~e <br />to one tical of the colder clo~ Under the5~ <br />particular conditions, cloud seed n has the poteli- <br />tial of substantially increasin~ the rate.of precipi- <br />tation. probably by as much as a hundred percent. <br /> <br />-I. <br />I <br />, <br />\ <br />i <br />I <br /> <br />The Colorado River Basin Pilot Project vas designed <br />as a statistical te9t of the capability of the cloud <br />seeding technology of 1971 to bring about precipita- <br />tion increases. When the weather forecasters expected <br />stormcloud cond~tions considered favorable for seeding <br />_within a twenty-four hour period.beg~nning at 11 A.M. <br />(and!if established safety criteria were met). an <br />"experimental day" was declared. A random..1zed deci- <br />sion then was made Vhether ,th~ experimental day'would <br />be seeded or left" unseeded as a cootrol-. The experi- <br />ment was 10tended to run for four consecut.ive 'lrlnters- <br />and accumUlate 160 experimental days about eqUally <br />divided between. seeded and unseeded. It actually <br />ran for fll1e w1Dters and accumulated 71 seeded and 16 <br />unseeded days. <br /> <br />It was thought that the snowfall on seeded days nd~ht <br />~xceed that 00 unseeded experimental da s b about 15 <br />percent an puss y up to 30 percent,: and that.ex- <br />perimental cl~~~ might account for as much as half of <br />the season'n~nowfall. This would have corresponded <br />to a maximum preci?1tation increase of about 7.5 per- <br />cent for the season as a whole. Although evaluation <br />is not yet complete. ~rel~m1nary results indicate <br />that no such sIzable overall increase was realized. <br /> <br />There appear to have been many "unseeded" days itlll:le- <br />diately following seeded days when silver iodide <br />smoke. trapped in the valleys upwind of the mountain <br />range. affected the clouds and effectively caused <br />these daY9 to be seeded. On other days strong winds <br />carried t~e seeding effect over the ~ountain ~rest <br />and outside the study area. On still other days. <br />~__ . _.. 1.___. _ . <br /> <br />y <br /> <br />designated as "seeded," th.e silver iodide failed fa"" <br />one reason or another to ~each the clouds. On stili <br />other occasions the forecast of favorable conditions <br />vas unfulfilled or else fulfilled for only a portion <br />of the 24-hour period. so that any seeding effect was <br />greatly diluted. <br /> <br />,. <br /> <br />! Nevertheless there exists an identifiable subse~ of <br />i experimental days~ free from these disturbinR influ- <br />I ences. for which substantial snowfall increases <br />r "could be identitied with ,~ high deRree of confidence. <br />I <br /> <br />The tentative conclusions from the project character- <br />ize it as a limited success. It revealed serious <br />weaknesses at the 19/1 tecnnology in the methods used <br />to identif "seedable" occasions and. to place tne <br />seedin2 material in the desired place at the eSired <br />~. It failed alsO- to give a reasonably accurate <br />measure of the ~otent1al of cloud seeding for in- <br />creasrng the seasonal precipitation. On the other <br />hand. it furnished additional evidence that the under- <br />lyin~ principles are sound and that present veakness <br />has to do mainly with the practical difficulties of <br />effective application. <br /> <br />During the ~ive winter seasons of the.PIlot Project. <br />.32~ k~ ?f ~il~~r iodide. containing 147 kg of silver, <br />were dispersed. An unknown proportion .of'"1"t"'\i~s .de-:. <br />..posited on the ground or .on vegetation near the gener- <br />ator sites; a further unknown proportlon vas carried <br />to one side or the other "of the stuQY area or deposited <br />with precipitation either upwind or downvind from the <br />study area. or escaped precipitation processes and <br />recaioed suspended in the atmosphere. An estimate that <br />10 kg of silver actually.accumu1ated..~~thin the 340.000 <br />hectares of the study area appears reasonable. an accu- <br />mulation of 0.04 grams per hectare season. The current <br />preliminary estimate of average snow. accumulation in <br />the study area for tbe five years amQunts to 65 cm <br />water-equivalent per season. If 25 percent of this <br />fell from seeded storms. this amounts .to about 0.003 <br />gm of silver per heetare .per centimeter of seeded pre- <br />e1p.!tation. . <br /> <br />1 <br />i <br />! <br />I <br /> <br />Dur1Da the five years of the Colorado River Basin Pilot <br />project. there yas.a midwinter dip in the frequency of <br />storms suitable for seedins. corresponding to mean .. <br />upper-air temperatures too 'cold for "seedability." The <br />experiments did not establish with a reasonable degr~ <br />of confidence whether precipitation increases would <br />appear as prolongation of snoviall durations or as in- <br />creases ot lntenSlty. or both. Many such questIons <br />can be answ~red only by further experimentation. <br /> <br />HoYever. the results sUKgest strongly that the snovfaIl <br />climate under seedln~ will differ irom the natural cli- <br />mate only in very subtle ways that can be distinguished, <br />if at all. only by sophisticated statistical analysis. <br />That seeded.snowfall will be in any vay strange. either <br />as perceived or as it interacts with the natural en- <br />vironment. is now considered extremely unlikely. <br /> <br />The San <br />for tbe <br />seeding <br /> <br />Juan Ecology Project. did not include studies.of tbe techniques.o1_cloud <br />remainder of this volume. we asked the Bureau of Reclamat~on to provide <br />activities. which they considerately provided. <br /> <br />~~'eding.. .bu~ co. set. the '5:"ta~ii <br />an overview ~f the. cloud <br /> <br />;18' <br />
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