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<br />. <br /> <br />SOME STATISTICAL TOOLS IN HYDROLOGY <br /> <br />21 <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 and 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 />. <br /> <br />The assumptions 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 basis, 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 />. <br /> <br />Y =a+bX. <br /> <br />The second (upper right) requires <br /> <br />Y=a+bX+h,X', <br /> <br />where the direction of curvature determines <br />the sign of hi' The third plot (lower left) indi- <br />cates the need for a transformation unless the <br />divergence can be explajned 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 another <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 />y <br /> <br />/" <br />.. <br />, , <br />, , <br />,'. <br />" . <br /> <br />x <br /> <br />x <br /> <br />y <br /> <br />.' <br />, <br />'. ' <br />... . <br />:: .0. <br />~ . .. <br />00.. <br />.' , <br />.. . <br /> <br />, . <br /> <br />y <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 =j(X), <br />and another for X=j(Y) (fig. 15). The struc- <br />turalline, which balances the plotted points in <br />both directions, has 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=j(X), <br />(1) group the points by small increments of X, <br /> <br />. <br /> <br />y <br /> <br /> <br />Y=o'+O.53 X <br /> <br />x <br /> <br />Figure 15.-Plot showing the two regression lines and the <br />strudurol line. <br />