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<br />, <br /> <br />ERNAL USE ONLY <br /> <br />~ I' \It 1\0 \? <br /> <br /> <br />Arkansas Valley in Colorado <br /> <br /><::> <br />o <br />N <br />~ <br />I-" <br />-.l <br /> <br />Suggestions for Q~t~"':-l~tical analysis <br />oi histoi~~Jl records <br /> <br />Introduction <br /> <br />Two appro,::,::,c:12S seem appropriate in the c..n&lysis or historical'records. <br /> <br />(1) River llgainll and (2)"system 10ss.1T The accompanying d:.agram~ic sketch <br /> <br /> <br />may illustrate my idea. The sketch is very greatly over-s~:;l/~ified, needless <br /> <br /> <br />to say, but may be adequate to demonstrate the difference b2cween the two <br /> <br /> <br />approaches.. Both approaches \ViII be handica.pped by the complete lack of ,some <br /> <br />data, and in<lCCU1~ac:~,..s and incomplct;12SS oE ",".v.s.ilable data~. For example, records <br /> <br />of histori.::al chat:2;2s in gr"und-wate:r storage are virtually nonexistent; pre- <br /> <br />cipit~tion reco~ds a~e not detailed enough to be more than a crude measure of <br /> <br /> <br />amounts and s?atisl distribution] a very few of items B, C, and G have been <br /> <br />contin~ously ffie.:lSUrcJ since only about 1940; item F can only be estimated; <br /> <br /> <br />there ~re no h~~:orical records of underflow. However, preliminary analyses <br /> <br />have encou:r.::ged'me to the extent thai.:. I would recommend fu:cc:her investigations~ <br /> <br />r::..:., inv<2st:.g.:.rte river "gain", the dependent variable shoul0 ~e H+D+E-A-C-G, <br /> <br /> <br />durir: ~Jeri.o~':'s ;,:hat they were all measured. The 0ependent var iable for system <br /> <br />Hloss;/ should 0<=. A+B-F-H. The independent variables in both investigations <br /> <br /> <br />shoulc De: suriace water applied to lands within the systero; water pumped <br /> <br /> <br />from c~a valley fill; and precipitation. Logically, some measure of solar <br /> <br />radia~~on also should be considered, but similar investigations I have made in <br /> <br /> <br />the p~_oc r0~ch have indicated that; first, there is undue correlation between, <br /> <br /> <br />for e~~~ple, ?an evaporation at John Martin, and precipitation; and second, <br /> <br /> <br />that the ra~lge - from year to y-.;;ar - in total radiation is too small to warrant <br /> <br /> <br />its i~clusi0n as a variable. <br /> <br />, <br /> <br />',:", <br /> <br /> <br />T:'12 pitfalls - and pratfalls - in using multiple regression analysis are <br /> <br /> <br />too Hc..:~_ kr.own for me to elaborate, except to say that we will not obtain <br /> <br /> <br />absolu::..:: proof of anything. I am almost certain, though, that c;:rc::ul considera- <br /> <br />tion of ~he results of mathematical analysis of historical' datn w~:: give us a <br /> <br /> <br />much better understanding of the system - and of data deficiencies v <br /> <br />',', <br /> <br />1 <br /> <br />,'. -~,.< <br /> <br />.-. <br /> <br />'"'' <br />