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• inflection points neaz 8.5 and 11.5 inches of precipitation. The calculated correlation <br />coefficient is 0.4781, with the best equation explaining less that fifty percent of the <br />variation in the data. Plotting total cover data from the individual reclamation years <br />reveals best-fit curves with correlations of one (Figure 18). Unlike the curves derived <br />from the older reclamation areas (1985, 1986, and 1987) for cover and precipitation, the <br />curves for the younger reclamation areas reveal that while the results from individual azeas <br />aze consistent, the overall response to precipitation is significantly broad in the younger <br />reclamation, explaining the poor correlation when these young reclamation areas aze <br />plotted together (Figure 17). <br />Total vegetation cover and September-July precipitation for the 1995, 1997, and 1998 <br />reclamation azeas is shown collectively and individually in Figures 19 and 20. As with the <br />January-July plots, the collective plot reveals a third order polynomial as the best-fit curve <br />with two inflection points in the data range. A correlation coefficient of 0.4781 was <br />obtained for this data set. Again, individual plotting of the 1995, 1997, and 1998 <br />reclamation azeas total vegetation cover and September-July precipitation shows <br />individual correlation coefficients significantly higher than the collective plot with second <br />and third order polynomials. While the plot of overall and individual reclamation area <br />responses to the precipitation regimes reveals best-fit curves consistent with that expected, <br />the variability of the younger reclamation areas is evident in the low overall correlation <br />coefficient. <br />• Total Herbaceous Production <br />The results of curve fitting for the two precipitation regimes and total herbaceous <br />production for the 1985, 1986, and 1987 reclamation areas are found in Figures 21 <br />through 24. <br />The plot of January-July precipitation and total herbaceous production data from the <br />1995, 1997, and 1998 reclamation areas from 1998-2001 is depicted in Figure 21. The <br />closest fit curve is a third order polynomial with a high correlation coefficient <br />(RZ= 0.8583). As was the case with cover data, this represents a significant improvement <br />in the explanation of variation from that of the closest fit curve for all reclamation azeas <br />and total herbaceous production (R2= 0,7396, Figure 4). Figure 22 depicts the best-fit <br />curves for the 1995, 1997, and 1998 reclamation azeas data individually and as with total <br />cover in the younger reclamation areas, variation in the individual reclamation areas is <br />great in terms of curve type, shape, and general form of the best-fit curve. The best-fit <br />curve for the 1995 reclamation area is a third order polynomial, for the 1997 reclamation <br />azeas an exponential, and the 1998 reclamation areas a straight line. Correlation <br />coefficients for the 1995, 1997, and 1998 areas varied widely, from one in the 1995 <br />reclamation azeas to 0.135 in the 1998 reclamation azeas. As with the cover plotting <br />described above, this result is indicative of the wide variation in response of the younger <br />vegetation in these reclamation areas. <br /> <br />-> a <br />