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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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Template:
Weather Modification
Applicant
Western Weather Consultants
Project Name
Vail Pass
Date
11/1/1984
Weather Modification - Doc Type
Application
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<br />" <br />. <br /> <br />.1 <br />~~ <br />:1 <br />.~ <br />I <br />, <br />.; <br />I <br /> <br />; <br />i <br />I <br /> <br />I <br />\ <br />! <br />I <br />'I <br />.j <br />.i <br />:i <br />i <br /> <br />'," <br />, <br />'. <br /> <br />; .~ <br />"-~ . <br /> <br />:\ <br />\, <br /> <br />.. <br /> <br />.~ <br />. <br />I <br />I <br />i <br />.~ <br /> <br />J <br /> <br />, <br />. <br />.. <br />I <br />l <br />:,~ <br /> <br />CHAPTER It <br /> <br />y <br />A DISCUSSION AND SYNTHESIS <br /> <br />INTRODUCTION <br /> <br />NeJ CallH' - . C. P. Patrick Reid, P_ J. Webb.er. and Donald A. Klein <br />, <br /> <br />This chapter Is intended to dra~ to~ether the main <br />conclusions of Chaot€r IV of this report vith <br />regard to the influence of cloud seedin~ on the <br />terrestrial ecosystems of the San Juan Mountains~ <br />:Following a brief description of the field area. the <br />ecosystem components are considered separately and <br />then the possibility of linked interactions among <br />them. vhich may lead to either"damped or amplified <br />responses to snawpack augmentation. Is discussed. . <br />This treatment requires some speculation about poten~ <br />tial impacts, especially long term oneS, since not all <br />of the predictions made hare are based upon statis- <br />tic:.aJ.ly' proven relationsh.1ps_ The 'speculation is. <br />. however. that. of scientlsts who have 'WOrked in the <br />'.-; San Juan Kounu.iD8 for 5 years and so is usefully <br />included in a general discussion of ecological <br />effects. bearing in mind the increased risk of error <br />whi..ch such speculation entails. <br /> <br />During: the 5 yeat: life of t.he -re.search. ~epo-rted <br />bere (1910-1975). the San Juan Mountains have <br />. ; been the site of a pilot project designed to test <br />the- .operational effectiveness of snowpack augmenta":,' . <br />tlon through a randomized seeding experiment. <br />Originally. it was anticipated that the project <br />vould ~ive e. 15 ~e'rcet\t inC'rease. in vinte-c snovpac.u; <br />that is ahout one half of the expected full poten-. <br />tial of vincer cloud seeding 10 the area. ~ubgequent <br />evaluation of t.he cloud deeding eX{Jed.l1lenc has led to <br />the conclusion that actual snowp8ck augmentation vas <br />below the anticipated 15 percent level (Howell. this <br />vol~ p. 5). Any aytlficially caused increase in the <br />saawpack of the San Juan Mountains has been imposed <br />on a region in which prec1p1tation and snow <br />accumulation is naturally n1ghly var1able: annual <br />snowfall there ranges between 35 percent less and <br />~~U ercent greater than the annual mean ot 4U cm <br />'Water equivalent V.e-. measured ove-r a year <br />period. ~ny of the estimates of ecologic impact <br />made in tbis study are based on the potential 30 per- <br />cent increase in me-an snovpack accumulation that vas <br />originally ass~ed to be possible in an operational <br />phase .o:f winter cloud seeding. <br /> <br />TIlE FIEUl AREA <br /> <br />In southwestern Colorado. tbe Continental Divide <br />makes a wide bend to the west around the headvaters <br />of the Rio Grande and through the San Juan Mountains. <br />The target area for cloud seeding has been a 3400 km2 <br />area in the southern and eastern part of the range, <br />extending from the Colorado-New Mexico state line to <br />the Needle Mountains. Most of the field ..investiga- <br />tions of the San Juan Ecology Project have been <br />conducted in this target area (Figure 1. Chapter I). <br /> <br />In the target area. the Continental Divide runs almost <br />east-west and subsidiary ridges extend from it to the <br />south or southwest betveen tributaries of the San <br />Juan River. The topography of the area is generally <br />rugged with some of the peaks ~xceeding 4250 m ele- <br /> <br />vation. With the exception of Wolf Creek Pass, no <br />all-weather roads cross the mountain area and ~uch <br />of it lies within the Weminuche ~ilderness. <br /> <br />Geologically. this is a young pa'rt of the southern <br />Rockies and is. composed 1a'rgely of Tertiary volcanic. <br />tuffs and lavas, although metamorphic mater13ls of <br />Precamb'rian age are exposed extensively in the ~eedle <br />Mountains and G'renadier Range at the ~estern end of <br />thp. target area. Mesozo~c sedimentary materials are <br />found only at lover elevatlons.- This diversity of <br />paren~ materials, combined with the changes of <br />cl1ms~e and vegetation due to elevation and a his- <br />tory of multiple late-cenozoic glaciations, has- <br />pyoduced a complex pattern of 8011s and surficial <br />deposits; however. this complexity is typical of <br />th:e southern Rocky Moun~ains. , .ff' <br />Sec.,-r""n4: _,Q"... ed..,- <br />- cm~:Ct..iJsiONS . 'd" . <br /> <br /> <br />. ~ :;i;.",: :):~ .....--::. .-" <br /> <br />The results of-the San Juan Eco!o~Y Proiect sU~Rest <br />that there should be no. in::mediate. larlOl:e-scale <br />l~oacts on the terrestrial ecosyst~ of these . <br />mountains followi~ an addition of up to 30 percent <br />of the. normal snowpack, but wit no ad t on to <br />:- r.axitDUtlI. sno\lj)8cks.. ..Further. ouch of the vork re- <br />.;ported here SUl:!:l:!:ests that compensating Dec..~an1sms <br />'~itnin the studied ecosysteQS Rre such that any <br />i~?acts vould be buffer~d. at leas~ fur short periodS <br />~. of time. and of lesser.ma~nitude than the changes <br />,~, in snow conditions required to produce them. <br />~-:"i .' :'; _ ", '"__ ..' . <br />HoYever~ some parts of the mountain ecosystem ~re <br />much more susceptible to chanRes in 9noy conditions <br />~han others. so important local effects are ~ossible. <br />In general. these susceotible components n~e very <br />small parts of tbe entire system but their economic <br />or esthetic value may be much greater than their <br />mass or area SURRest. Remedial action is possible <br />in most. of these cases but has not been studied ln <br />this project., Our work has shown three eCOsystem <br />c onBnts to be most susceptible to inc'reased <br />snowfall: snowbank situations at elevations above <br />treeline; (2f elk herds (in other mountain ranges <br />~other big game spec1es may be simil~rly affected); <br />and 3) some-small mammal populat!ons~ especially <br />the deer mouse. Not all of these impacts are <br />. necessarll deleterious; an increase in the area of <br />snowbank edge habitats in alpine area may~ or examp e, <br />increase the niches available for rare plant species. <br /> <br />,. <br /> <br />ina!l even ln the small 8'reas where 'we predict <br />rea test impacts from inereased snow ate c anges <br />nvolved a're un i e y to approac t e magn u e 0 <br />at e'r man-ma e mpacts on mounta n ecosystems. ow- <br />eve'r. it 6nou~d be rememberea tnat tney may act in <br />phase vith other man-made impacts and with natural <br />climatic changes. in which case the total effect <br />could be much greater than our studies suggest. <br /> <br />.~ . -,....- -~,._~'-- <br /> <br />:-' .ll ~ Ste-l1'1ho-ff~:-Harold-Y-"':,and':Jack-D:-lVe6--{Ed~.)~1976-.- Ecp:l!>8-ic~l impacts of snO\lPack augr..en~<!.tit,l', i.n l'\~ <br />. San Juan Kountains.-- Colorv.do: Final Report, San Juan Ecology Project, Colorado State Univer:!dty l'u::l.; <br />Fort Collins. <br />!I Present Address: INSiAAR. University of Colorado. Boulder. Colorado 80309. <br /> <br />-29- <br /> <br />A-13-5 <br />
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