Laserfiche WebLink
<br />GENERAL PROCEDURE FOR GAGING STREAMS <br /> <br />By R. W. Carter and Jacob Davidian <br /> <br />Abstract <br /> <br />This chapter brielly describes the objectives and pro- <br />cedures used in obtaining streamflow records. It is <br />consideri:'d an introduction to other chapters on sur- <br />face-water techniques which treat individual prore- <br />dures in greater detail. <br /> <br />Introduction <br /> <br />Measurement of the flow of streams was be- <br />guu by the U.S. Geological Sur\'ey in 1888 as <br />part of special studies relating to the irrigation <br />of public lands. Since that time svstematic <br />records of streamflow have been obtained at <br />more than 16,lXlO places in the United States by <br />the Geological Survey. In 1967 the stream- <br />g-aging- network comprised about 9,000 continu- <br />oils-record stations. In addition. there were <br />about 7,200 p.trtial-record stations where data <br />on only ftoodftow or low flow were obtained. <br />Stream p;aging is the largest operation among <br />the ""rious hydrolog-ic networks. Streamflow is <br />the only part of thc hydrologic cycle in which <br />moisture i~ so confined as to permit re.tlsonu- <br />hly a{,L'Ul'ate measnrements of the volumes in- <br />volved. c\ll other measurements in the hydro- <br />logic cycle are at best only inadequate sa;llples <br />of the whole. <br />'Vater in streams serves mall in many ways; <br />it provides water supply for man and animals, <br />irrigation wruter for plants, dilution and trans- <br />port for removal of waste, energy for produc- <br />tion of power, channels for water transport, <br />and a medium of recreation. Records of stream- <br />flow are important in each of these uses. <br />\"ah'r in streams cnn nlso be a hazard. Floods <br />('lW1'*-' pxtt~llsin~ dUllIug'e and hardship. Records <br />of fto(}(l (.y(.]}ts obtailll;'(l at :,!ag-illg' :-:otatioHs Sf'l'Yl;' <br />as tIlt'- basis fol' tIll' ell'sign of highwllY bl"id~~ <br />and eHln~rts, (lalll~, and f1oO(l~~'ontrol reSl'l"\"Oil'H <br /> <br />l~~ <br /> <br />and for flood-plain delineation and flood- <br />warning systems. <br />The network of stream-gaging stations is de- <br />signed to meet the various needs for informa- <br />tion on streamflow. MallY stations are operlVted <br />to provide current information for use in the <br />day-by-day management of water supplies or <br />for use in forecasting flood events. Most of the <br />"t"tions, however, are operated as a pam of the <br />hydrologic network. Records for these stations <br />reflcct the natural hydrologic characteristics of <br />the basins and can thus be used as samples of the <br />variations of streamflow in time and space. <br />The design of strCltmflow networks is gov- <br />erned to some extent by the nbilit.y to measure <br />stage and rliselULrge at a given site to the re- <br />quired degree of accuracy. The continued de- <br />velopment of new instrumentation and analyti- <br />cal techniques has improved the capability of <br />obhtining streamflow records under difficult <br />eonditions. <br />This chapter describes in general terms the <br />t-edlniqlles used in obtaining- eontilluouS stream- <br />flow re,'ords-- from selection of site to publica- <br />tion of records. H is considered an introduction <br />to four other chapters in book 3, section A, <br />surfnce-water techniques, which describe in de- <br />htil the instrumeuts and techniques used in <br />making specific measurements. This series of <br />chapters may be considered an updating of <br />Water-Supply Paper 888, "Stream Gaging <br />Procedure." <br /> <br />General Objective and Procedures <br /> <br />The objective in operating a gaging station <br />is to obtain a continuous record of stage and <br />,liselmrge at the sitc. The exact location of the <br />station is chosen to take advantage of the best <br /> <br />1 <br />