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Table 5-2. Regression model for political party entropy H(P) in the 1992 presidential election at the county level. |
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Table 5-3. Turnout-party entropy H(P) models for parliamentary elections in Western Europe and Canada; estimated slope coefficients for H(P) = a0 + a1t + a2t2 or H(P) = a0 + a1t and location of the maximum for the parabolic model. |
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Table 5-4. Turnout-party entropy H(P) models for Western Europe, New Zealand, and Quebec with party entropy controlled for number of parties k; estimated slope coefficients for H(P)/log2 k = a0 + a1t + a 2t2 or H(P)/log2 k = a0 + a1t and location of the maximum for the parabolic model. |
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Table 5-5. Turnout-party entropy H(P) models for Eastern Europe and Russia; estimated slope coefficients for H(P) = a0 + a1t + a2t2 or H(P) = a0 + a1t and location of the maximum for the parabolic model. |
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Table 5-6. The linear relationship between party entropy H(P) and turnout t in Japanese prefectures (N = 46): H(P) = a + bt. |