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Last modified
1/25/2010 7:15:03 PM
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10/5/2006 3:45:45 AM
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Title
Techniques of Water-Resources Investigations of the US Geological Survey Some Statistical Tools in Hydrology
Date
1/1/1969
Prepared By
USGS
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />SOME STATISTICAL TOOLS IN HYDROWGY <br /> <br />21 <br /> <br />. <br /> <br />able, all coefficients having the same sign, then <br />we would conclude that the effect of that vari- <br />able was real but, of course, small. <br />A distinction should be made between statis- <br />tical significance and practical significance. The <br />regression coefficient of a variable may test <br />highly significant, and yet the effect of that <br />variable on the dependent variable may be <br />negligible, <br />Uses o.nd interpretations of regression analy- <br />ses in hydrology have been discussed by Riggs <br />(1960) and Amorocho and Hart (1964). <br /> <br />Graphical regression <br /> <br />The sssumptions required of graphical re- <br />gression are the same as those required for <br />analytical regression. The results of a graphical <br />regression can be expressed mathematically if <br />no restrictions are added to the graphical <br />analysis, and the standard error can be <br />estimated, <br />Graphical regression is less restrictive than <br />analytical regression in that the model need <br />not be completely specified in advance. In <br />fact, f an analytical model cannot be selected <br />on' a physical bssis, it is conventional to prepare <br />a preliminary graphical regression which will <br />indicate an appropriate model. For example, <br />consider the four data plots of figure 14, The <br />first (upper left of fig. 14) indicates use of the <br />model <br /> <br />I' <br /> <br />. <br /> <br />. <br /> <br />Y=a+bX. <br /> <br />The second (upper right) requires <br /> <br />Y =a+bX +b,X', <br /> <br />where the direction of curvature determines <br />the sign of bl' The third plot (lower left) indi- <br />cates the need for a transformation unless the <br />divergence can be explained by an additional <br />variable. The fourth plot (lower right) shows <br />no relation between Y and X, and, if only a <br />two-variable relation is being considered, no <br />further analysis would be made. A relation, <br />however, between Y and X in the fourth plot <br />may be obscured by the effect of 8J)other <br />variable Z which has not been included. This <br />aspect is discussed on page 23. <br />The preparation of simple linear relations <br />between two variables is well known, The re- <br />gression line is not necessarily the same line as <br /> <br />y <br /> <br />, ' <br /> <br />/' <br />" <br />, , <br />, " <br />'", <br /> <br />," <br /> <br />y <br /> <br />/> <br />, , <br />, , <br /> <br />", " <br /> <br />x <br /> <br />x <br /> <br />y <br /> <br />"' <br />, <br />" ' <br />. , , <br />:: .-. <br />~ . ... <br />.- .. <br />" , <br />:. . <br /> <br />y <br /> <br />, , <br /> <br />x <br /> <br />x <br /> <br />Figure 14.-Four possible outcomes of plotting Yagainst X. <br /> <br />one would draw through the plotted points. <br />There are two regression lines, one for Y =f(X) , <br />and another for X f(Y) (fig. 15). The struc- <br />turalline, which balances the plotted points in <br />both directions, hss a slope approximately mid- <br />way between the two regression lines. The <br />differences in slope among the three lines depend <br />on the degree of correlation of the variables. <br />For perfect correlation all three lines have the <br />same slope. Regardless of the correlation, both <br />regression lines pass through the mean; the <br />structural line mayor may not pass through <br />the mean. <br />To approximate the regression Y=f(X) , <br />(1) group the points by small increments of X, <br /> <br />. <br /> <br />y <br /> <br /> <br />Y=o<rO.53 X <br /> <br />x <br /> <br />Figure 1 S.-Plot showing the two regression lines and the <br />structural line. <br />
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