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<br /> <br />Application of Stochastic Hydrology to Simulate Streamflow <br />. and Salinity in the Colorado River <br /> <br />~ <br /> <br />l'\) <br /> <br />Erratta: <br />September a5, 1975 <br /> <br />Equation 1a on page 20 should' read: <br /> <br />"- <br /> <br />0) <br />w <br /> <br />sj, · sj, - t, <br /> <br />j2~ J <br />S k . 2 2 <br />S~k Sxk - Sxn <br /> <br />.... <br />'" <br /> <br />The equatiqm was correctly quoted from the reference, however the <br />equation w4sincorrect in the reference. The effect of using this <br />wrong equation is that the adjustments to the upper basin flows are <br />in error. :For the purposes for which the simulation data had been <br />used, it is felt that these errors are not of great concern. However, <br />because it:isfelt that this error cannot be ignored, we are now <br />util i zing means and standarddevi ations computed prior to thi s <br />adjustment. <br /> <br />W"' <br /> <br />September 16, 1975 <br />The footnote .on page 15 should read: <br />1/ See references, page 38. <br /> <br />April 14, 1976 <br /> <br />There a. re sltrong reasons to bel ieve that the method of ana lysis and <br />generation pr~serves monthly means, monthly standard deviations, lag <br />one serial ~orrelations, but not completely lag zero cross correlations. <br />The interested reader is referred to "Mathematical Assessment of Synthetic <br />Hydrology" by N. C. Matalas in Vol. 3, No.4 of Water Resources Research, <br />1967. ' . <br /> <br />, <br /> <br />,_w" <br /> <br />:.'I'~..'.!i!i&.'.'.".. <br />;ell! <br />":-;"N' <br />:gi:'-~: <br />~V'".'f: <br /> <br />i~ <br /> <br />-i~:f~ <br />-~o:fji, <br />.~~to}::~~ <br />~~1~; <br />i;\;',;m <br />'if,I!t:.~f'!J. <br />~}!.^-;.."i1l <br />~-~.;~-m <br />~!^" <br />. .,.~" <br />;,).}:~__,tr: <br />f~'.-'~ <br />~~~~~ <br />" <br />I.f,." <br />>. ,.... <br />