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<br />I <br />I <br />I <br />I <br /> <br />FIGURES <br /> <br />l.--The Colorado River drainage basin. <br /> <br />2.--Mathematical programming form of the optimization of <br />the routing of hydrographers. <br /> <br />I <br /> <br />3.--Tabular form of the optimization of the routing <br />of hydrographers. <br /> <br />4.--Burkham-and-Dawdy accuracy analysis of streamflow data <br />for the Colorado River below Davis Dam. <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />5.--Theoretical error variances of real-time estimates of <br />discharge. <br /> <br />6.--Theoretical error variances of smoothed estimates of <br />discharge rate. <br /> <br />7.--Limit of bias introduced by approximating the error <br />variance of estimates of annual mean discharge. <br /> <br />8.--Residuals of discharge-rating analysis for the Colorado <br />River below Davis Dam. <br /> <br />9.--Autocovariance function of the differences between true <br />and rated discharge rate for the Colorado River below <br />Davis Dam for the water years 1956-1958. <br /> <br />10.--A comparison of Kalman-filter results with those of the <br />Burkham-and-Dawdy procedure for error estimation. <br /> <br />ll.--Schematic of the network of stream gages serviced from <br />the Blythe Field Office. <br /> <br />l2.--Schematic of the network of stream gages serviced from <br />the Yuma Subdistrict Office. <br /> <br />l3.--Autocovariance function of the differences between true <br />and rated discharge rate for the Colorado River below <br />Davis Dam. <br /> <br />I <br />I <br />I <br />I <br />I <br /> <br />l4.--Standard error of estimate of annual mean discharge for <br />the Colorado River below Davis Dam. <br /> <br />lS.--Autocovariance function of the differences between <br />true and rated discharge rate for the Topock Marsh <br />Inlet near Needles, Calif. <br /> <br />iv <br /> <br />Page <br />2 <br /> <br />11 <br /> <br />12 <br /> <br />16 <br /> <br />26 <br /> <br />29 <br /> <br />32 <br /> <br />36 <br /> <br />38 <br /> <br />40 <br /> <br />43 <br /> <br />44 <br /> <br />47 <br /> <br />48 <br /> <br />50 <br />