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. 2013 Oct 11;8(10):e76872. doi: 10.1371/journal.pone.0076872

Table 1. Scaling exponents (α) and intercepts (β) of M-A relationship at six altitudes as estimated by RMA regression.

Altitude (m) Latitude (N°) Longitude (E°) α 95% CI of α β 95% CI of β R2 Sample size
414 119°26.41′ 30°19.61′ 0.859 c 0.780, 0.946 −2.103 −2.249, −1.957 0.823 78
620 119°26.24′ 30°19.90′ 0.963bc 0.853, 1.088 −2.248 −2.463, −2.033 0.642 97
850 119°26.00′ 30°20.24′ 1.000b 0.912, 1.097 −2.374 −2.541, −2.206 0.704 138
1086 119°26.03′ 30°24.49′ 1.113ab 0.974, 1.273 −2.473 −2.541, −2.206 0.640 81
1286 119°25.67′ 30°20.64′ 1.299 a 1.160, 1.455 −2.868 −3.114, −2.623 0.773 72
1462 119°25.51′ 30°28.90′ 1.258 a 1.161, 1.364 −2.821 −2.993, −2.649 0.839 99

All regressions were significant (P<0.05). Boldfaced slopes are statistically significant different from 1 at P<0.05 level. The Post-hoc multiple comparison of slopes were shown among altitudes, where the slopes sharing the same superscript letters are not significantly different from each other at P<0.05 level.