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to <br />Iu <br />J <br />LL <br />U <br />N <br />a <br />_Z <br />4 Pr ? <br />5 <br />HYDROLOGIC REGIONS <br />FIGURE 5. Mean August cfsm comparisons of <br />eight hydrologic regions. <br />gage sample size (n = 3) and the wide fluc- <br />tuation of August discharge data charac- <br />teristic of that region created a high degree <br />of data variability. The wide fluctuations <br />in this region are caused by severe August <br />rainfall events, including hurricanes that <br />historically do not occur as intensely in the <br />Mt 3 <br />95% COMMENCE WERVVALS <br />FOR EACH REGION <br />IC„ <br />I n=3 <br />rr2 <br />rt3 <br />?u 1 re4 n a <br />111 I1 <br /> <br />other regions. Additional unregulated gage <br />data from this region would be required <br />to draw statistical conclusions regarding <br />August flow regimes. Unfortunately, no <br />additional gage data for unregulated <br />streams appear to be available at this time. <br />A model II one-factor Analysis of Vari- <br />ance (ANOVA) was performed among all <br />eight regions (49 gages), the Scheffe F-sco- <br />re results of which indicated that signifi- <br />cant (P < 0.05) differences exist among at <br />least some of the regions. Paired ANOVA <br />comparisons among the regions indicate a <br />pronounced difference between the moun- <br />tain windward region and nearly all other <br />regions (Table 4), despite the use of the <br />Scheffe test, which is very conservative (i.e., <br />it makes it difficult to find significant dif- <br />ferences). Significant differences among <br />other pairs of regions were not pro- <br />nounced. <br />Although a total of eight hydrologic re- <br />gions were identifiable based on physical <br />basin characteristics, only two region sets <br />could be statistically distinguished. Figure <br />5 and Table 4 reflect that drainages on the <br />windward sides of mountain ranges form <br />a separate hydrologic group from the other <br />seven regions and suggest that 1,200 feet <br />elevation is close to the critical mean basin <br />elevation, separating mountain from lower <br />elevation drainages. <br />A comparison between mountain wind- <br />ward and other regions (mountain lee- <br />TABLE 4 <br />ANOVA F-score comparisons among eight New England hydrologic regions <br /> Mtn. <br />wind Mtn. <br />lee Int. <br />west Int. <br />cent. Int. <br />east L. I. <br />Sound Gulf of St. <br />Maine Law. <br />Mountain-Windward - <br />Mountain-Leeward 13.02, <br />Interior-West 3.23, 0.51 <br />Interior-Central 9.82, 0.44 1.22 <br />Interior-East 10.72, 0.02 0.60 0.25 <br />Long Island Sound 2.28, 0.55 0.01 1.23 0.63 <br />Gulf of Maine 2.02 0.23 0.01 0.72 0.29 0.01 <br />St. Lawrence 1.71 0.90 0.07 1.64 0.98 0.03 0.07 - <br />Source df Sum squares Mean squ are F-test <br />Between groups 7 0.971 0.139 18.755 <br />Within groups 41 0.303 0.007 <br />Total 48 1.274 <br />'Significant at 95%. <br />I B. H. Kulik 19 Ir_?_