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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 />000591 <br /> <br />quently in response to changing conditions. Accuracy goals at a given site <br />depend on the requirements of a particular management system, and can be <br />met by intensive observations or by more sophisticated instrumentation as <br />needed. <br /> <br />Data for Planning and Design of Water Projects <br /> <br />The goal for this type of data is to define with appropriate accuracy <br />the statistical flow characteristics for all streams in Kansas. This <br />includes not only all streams with natural flow, but also those streams <br />that are affected by regulation and diversion. <br /> <br />Accuracy goals in this report are defined in terms of accuracy of <br />statistical characteristics of streamflow, rather than accuracy of basic <br />data such as individual discharge measurements or daily flows. Except for <br />a few stations with unusual problems, accuracy of the basic data Is ade- <br />quate for use in determining statistical characteristics; accuracy of <br />statistical characteristics is limited almost exclusively by the length of <br />streamflow record. <br /> <br />The principal measure of the accuracy with which a particular stream- <br />flow characteristic can be determined is the standard error, expressed in <br />this report as a percentage of the estimated value of the characteristic. <br />For flow characteristics (except standard deviations of annual and monthly <br />flows) calculated from streamflow records at a particular site, the <br />standard error can be calculated from a theoretical relation of standard <br />error to variability index (standard deviation of the logarithms of the <br />data) and number of years of record. For standard deviations of annual <br />and monthly flows, the standard errors, In percent, can be calculated only <br />from the number of years of record. In general, the longer the record, the <br />more reliable are the estimates of probable future occurrences. However, <br />even with a long record, 50 to 100 years', It is not possible to determine <br />flow characteristics with great precision. <br /> <br />The standard error of a streamflow characteristic decreases with years <br />of available record, but at a decreasing rate as shown In table 2. For <br />both natural and regulated principal :streams, the Importance and multiple <br />uses of data justify high accuracy so the proposed goal Is an accuracy <br />equivalent to that obtained from 25 years of record. For the remaining <br />streams, accuracy equivalent to that obtained from 10 years of record is <br />proposed as the goal. These goals apply to streams wIth natural flow and <br />to streams affected by regulation and diversion. For the latter case the <br />flow characteristics to be defined are those that reflect present condi- <br />tions of development. <br /> <br />Long-Term Streamflow Data <br /> <br />The goal for this type of data is to operate Indefinitely a small net- <br />work of stations for streams that are expected to remain relatively free <br /> <br />15 <br />
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