Laserfiche WebLink
<br />-. <br />.. , <br /> <br />Part 2 - Streamflow Data (Contd) <br /> <br />and into a seotion in Kansas from the State line to Garden City, whioh <br /> <br />is further divided into sub-seotions above and below the Syracuse <br /> <br />station. <br /> <br />The unconsumed outflows frmn the drainag6 basin upstream <br /> <br />from a gaging stet ion constitute the inflows at the head of the river <br /> <br />section next downstream therefrom. These measured inflows at the head <br /> <br />of a given river section a~ diminished by diversions from the river <br /> <br />along the section, and at the same time are augmented by tributary <br /> <br />contributions and return flows and other inflows to the river, and are <br /> <br />depleted by natural losses of water incident to its conveyance through <br /> <br />the section of river to the lower station or point of outflow therefrom. <br /> <br />". <br /> <br />Streamflow data assembled in Tables 1 to 9 are summarized by <br /> <br />months, seasons and years, as averages for the 1908-1942 study period, <br /> <br />in the following summary Table A, in which the stations are grouped in <br /> <br />accordanca with their locations above and below Caddoa. <br /> <br />Summary Table B shows the total stl'eamflow, including floods, <br /> <br />each year of the 1906-1942 period, for river stations above and at Caddoa, <br /> <br />from Table fJ 1-51 and summary Table C shows similar information for river <br /> <br />stations at and below Caddoa, from Tables 5-9. <br /> <br />Streamflow. data for the Canon City and Pueblo stations shown in <br /> <br />Table s 1 and 2, and in following sum,nary Table If A IUld B. include quanti ties <br /> <br />of water imported from the Colorado River systsm (Table 10). In the <br /> <br />following summary Table D these imported quantities have been deducted <br /> <br />. <br /> <br />-9- <br />