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<br /> <br />suggests the dedin€' ot salinity "oncen'ril.liQn<; may h<l'/€ he"'n in part r<lIIS".-j <br />by the transition f1"om a telativ~dy drier period (1055-65) "w'ilh ,111 _Hlnllcd <br />vir~in (unr1eplt"ted) fl.,.... of 13.23 ",illian acre-f"'Pt ;p L€'l?'5 Fen\'. t.., .f <br />telativel:; :,..'ptter period (19fJ5 75) '.'jlh;1Il <lnll'Jal ':il.';'111 fIr,... "f h.1f) miJlj"n <br />acre-feet. This is an increase in the tlw.' 0f arrln:~im,pply In PPI '-,tJf "1<1 "',~. <br />be responsible for a por~ion of the d€u"'A:O::~ ill "hE' s.llinl", r:nnr-t'ntlHj"n <br />observed at I~pel ial Dam. <br /> <br />~ <br />r.::: <br />'1 <br />r.. <br /> <br />The ":lore tecellt period (l'l8~ A7) ':.15 e'.'pn '!lOle extreme, '.dth :';omE <br />flo'_'s ':ell above rhose e....er lecorrieri. This "_';j~ proh<lbl,v the majol L,W"e at <br />the near 200 mg/L drop in salinity o'/I='r the Llst fe".. :.'''''U'';. ;. n,1fISlic<l1 <br />analysis r)f the CRSS projec':ons for salinir:. indicat""s tha! ';illinit"l '.'ill <br />usually l.ange bet'.'een 64":' and l,n..... "!g, L. 'w'i th an aVE'lage ot 8Jo m~/L lrndel <br />the present le'.el of de\'t:'lopmellt; ho'."e...er. ahout 5 pelC~n( of the time <br />salinity could ~ary outside this range, as it did in 1986 ~ith a salinity of <br />577 mg/L. <br /> <br />2. Reservoir Effects <br /> <br />One of the most significant ch,:lIlges '..hich h~s Or:clltrerj to th~ <br />salinity of the Colorado Ri'/fOr is due to the IP~ndation of the n",tut-al fIn\,! of <br />the rivet basin. One study 13/ sho....s that stol<\lZ:e in Lake rn1.rell reduced the <br />month-to_month '/ariiltion from thE' mean salinit\! hplo'.r r.len Can:..rnn [),~m frr)m 2')0 <br />mg/L to 72 mg/L. This is leadily apparellt in a plot of tile data, Figure V-J. <br /> <br /> "00 <br /> 1300 <br /> I~OO <br /> 1'00 <br />- <br />"- 1000 <br />. <br />- gOO <br />- <br />?; 800 <br /> 700 <br />- 600 <br />. <br />~ <br /> 500 <br /> '00 <br /> 30e <br /> :00 <br /> <br />. . <br />. : . :'. :'.' <br />~ ,.... . '. ~ . '. ... .. .. <br />'.:-- ,. .". <br />.. '. .'... ..... <br />. . ". ..... '.:.. , .., <br />.... '. "': '. :-:.. .' .' , .... <br />. . . ~.. ." .:." . <br />':,." ., '.. No' <br />..' . <br /> <br />'. <br /> <br />. . <br />,,( ,: t, <br />'., ;-:.::....\.... U/~..~ <br />(, . """...,\~ . . <br />, tJ... '..to <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 /> <br />. <br /> <br />19"0 <br /> <br />1950 <br /> <br />1960 <br /> <br />l-~:O <br /> <br />'980 <br /> <br />1990 <br /> <br />You <br /> <br />Figure V-J, Monthly salinIty belo1.r Lake Po~ell (l~~l 8'l. <br /> <br />The period of P63-80 reptesents the ~OSt significant period of <br />reservoir storage in the history of ':ater de.....elopment on the Colorado River. <br />Storage in F'laming Gorge Reser','oir. Laloe Po....ell. and Lake Mead increaseci froltJ <br />less than 20 million acre-feet in 1Q63 to o,'er 50 million acre-feet by IQ8f). <br />The spill of Glen Canyon Dam in lQ80 ended the initial filling of the major <br />reservoirs on the Colorado Ri',er. "'ate. ':hich 'w'as being used to fill the <br /> <br />'i-3 <br />