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<br />. . <br /> <br />3-3 <br /> <br />explainable? If there wer~ no significant differences, why weren't the data <br />pooled? If there arE: significc'lnt differences, does it invalidate the data <br />of the Co1oradoRiver collected by traditional means? If this is so, then <br />what fraction of the data bClse is unusable and comparable? <br /> <br />4. According to Tyus et ?of. (19b4), in dpscribin9 depths used by adult <br />Colorade sQua\'Jfi sh, "There was a si ani fi cant Idi fference (P = 0.01) between <br />Q<:P.ths rf'cordE':d from the Grepn RivE-rar,<1 i tSI'. tributaries (\':hitE: and. Yc:mpa <br />Rivprs)..." using radiotelemetry..di"ta. Does this invalicate pealing Green <br />al1G Yampil I\ivcr radiotelerr.etry depth da:.a as is cone in thp first H.U. <br />c~rvc? I <br />! <br /> <br />5. It only "vJithin chJnnel" i1abitct Sel€ttien is consiCf.red (item 4 of <br />ueta E.xcluded, p2cr 1), isn't an important part nf 1;.r!e rivrrinE:: he.bitat <br />beinq ignorpri (i.G., flooded woeclanos, f!lOOdCa bottor!1s, ('Iff-channel <br />b~ckwaters)? I <br /> <br />b. how Cen adulT: Coloraclo sGu(I,'Jfish in Ithe Colorc3<iO,.Grec-n eM 'fampa <br />Riv~rs ~xhibit siml1ar aEpt~ ana velocity prdterences (p?ges 1 ana 3) when <br />tre geomorpholcgy of tnf three rivers is so d~tferent? Tile Colorad.o has at <br />If:ast threE' rEoions (Elack Rocks, \':('st\-J~terJ (,?taract Lanyon) with water <br />dE.pth ot 6t tu' WU feet ~'ir.en:: scuc.lfi sh hav!E' bte;n found. The GrE'el1 and <br />Y2rpa Rivf:rs do not exhibit. slIch r!cpths. IJre r.;~tc. collected from thesp. <br />cnor~cleus r!?oions c'xcll1CE:c fron thE: e.ni'llys;s? I <br /> <br />_. _ 7. It cannot bp cenc 1 oded th'- t We ter d~Ptr- qrceter t>12 n ~. 95 ft. is a <br />'1mlt.lng factor. ~J'trOlJt extraDolc'tlng, .I'I'Clter Clcpth of 1..~5 :0 }(1.0 feet <br />rney b~ a lin;ting t<:lctcr (itr,f"'1 ~, f!ssur:pt;C\~S, pcgc 1). b!~c?USF' the datn <br />only inaic?te this rr;ngp of vclups. Colorc-cd souiH;lfish hove bl"p.n fOllnd in <br />(]~I='HIS grE'?ter then lC'.C fEet. here these dr.tlc1 excl llvrd fror'1 tf1f- iinalysi s? <br />I <br />E. ltfn 2 at ur:ta Utilizer' cr: pe~Q 4 is not clf,ar. \'ul~,iplyin? <br />rf-(crOfr rT:Pi"n co1u~r vt:10. citirs by t',;Jo, sir.cq JT!iCrCr'''bit2.,t vC'.loc;tics lJSt:C <br />by tilt: fish ..E:fA only ;>bcut l/~ thr r:<ean ct.lur;1f1 vC'loci-::y rt'(.rc:ser,tac by <br />c;sso(.iatl..:d CE:lls in tr')( Ly(1ri'ulic nO(:E-l, ir:C::ilcute:s ti:c USe of ttie inrlirect <br />pilrametE:r analysis. ~'Jas ttlr frecucncy (lnalysis uscd to ~eneri"t12 rhis curve <br />for nonspawninq velocity of acult SCUClwfish,1 or was a rOr'lbincti('lr, ot dcta <br />analysis techniques uspd? (see s€cticn 2.4 of Ithis aocUMent) <br />I <br />9. Th~ logic for not developing sUbstr8~e utilization cvrvps fer ~oult <br />nonspawning Colorado sQuawfish appears to be 1easonablf>, <br /> <br />I <br />2.2.2 Anult CclorrH~o s<1ua"Jfish steging poth, velocity and substrClte <br /> <br />1. ThE' depth p~ra~Pter for this cC\t~~ory and the 0f:nt"ratE'c1 li.U. curve <br />(p.,ses t - 7) appt:or to be' logically nerivE:'d.] hO\'Jcvpr, l'S in trH' trcatmf.'nt <br />on nonsp~.minc (irpt.rl, till do:;; arT lir.ited 10 10 f~~ft. ~,rc ttlfre c\'cper <br />~re~s used by st~cino scua~tish? ! <br /> <br />') . u . - , '1 f I 1 1" ( 8. ) <br />'- nO"J r;c tilL' moce e:r: rangC' 0 - 1n1'Cln "'J(lter co ur.m \'(' OCltH'S pagE' ' <br />r.or1rc:<rl..' ',-Jith cctudl tirlc 1Tc(!sun'mL'/lts? webs this rncen thilt fir' indirect <br />p?rCltTletcr ani\lysis .....;>5 p(:Y'torl1~ec? flo"'J mu~r. tield vnlidction h"'s this <br />hytiraulic ~odel r~ceivFd? ! <br />I <br />I <br />I <br />I <br /> <br />I <br />