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Last modified
1/26/2010 12:46:29 PM
Creation date
10/11/2006 11:18:06 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8407.600
Description
Platte River Basin - River Basin General Publications - Kansas General Publications
State
CO
Basin
South Platte
Water Division
1
Date
1/1/1970
Author
Kansas Water Resourc
Title
Evaluation of the Surface-Water Data Program in Kansas - 1970
Water Supply Pro - Doc Type
Report/Study
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<br />000589 <br /> <br />marked trend toward simulation of streamflow data based on the statistical <br />characteristics of flow during the period of record such as the mean, stan- <br />dard deviation, and skewness coefficient. <br /> <br />A long record of streamflow is the best basis for defining statistical <br />characteristics. Although it is not feasible to collect a long continuous <br />record at every site where it will be needed, a number of such stations are <br />required to provide information which can be transferred to ungaged sites, <br />or to sites where a small amount of streamflow data is available., <br /> <br />For natural streams the transfer of streamflow information Is done by <br />regression methods, either by relating flow characteristics to basin char- <br />acteristics such as drainage area, topography, and climate; by relating a <br />short record to a long one; or by interpolating between gaged points on a <br />stream channel. These methods are not applicable to streams where the flow <br />is affected by regulation or diversion. Because different techniques are <br />required to provide information on natural streams and regulated streams, <br />the two are considered separately in program design. <br /> <br />For regulated streams a systems approach is necessary if meaningful <br />information is to be provided. Operation of continuous gaging stations <br />defines the flow only at the sites of the stations but provides no basis <br />for prediction of future flows in time or at other points on the stream. <br />The systems approach req~ires an analytical model and detailed information <br />on the characteristics of the water management scheme 'that has been imposed <br />on the stream. These characteristics may include stage-capacity curves of <br />reservoirs, operating-rule curves for release of water, diversions of water, <br />and the channel geometry of the stream. <br /> <br />The required analytical models are simple in concept and will usually <br />consist of water-budget equations and flow-storage equations. However, in <br />many cases the use of the digital computer will be required for complex <br />computations, or to handle efficiently large volumes of data. A computer <br />program tailored to the individual system can be prepared. <br /> <br />Information on flow at some point or points on the stream is also <br />necessary. Fortunately, many of the stations operated for the purpose of <br />current data are on regulated streams and the records provide a base for <br />the systems study. <br /> <br />i <br /> <br />For the purpose of setting accuracy goals, streams are further classi- <br />fied as minor streams ~nd as principal streams. The intent is to use size <br />of drainage area as an index of value of data. More costly developments on <br />larger streams justify a higher accuracy goal for principal streams than, <br />for minor streams. The point of division between the two classes is a <br />drainage area of 500 sq mi, except in the western third of the State, where <br />streams draining more than 1,000 sq mi are termed principal streams. The <br />western third of the State includes al I the counties west of the tier of <br />counties from Phillips County south (figs. I and 2). This flexible defini- <br /> <br />II <br />
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