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.