Table 5. Response surface regression results and their F values at the four different elevations and the composite site.
Site | A00 | A01 | A02 | A10 | A11 | A20 | F | F0.01(5,49)/F0.01(5,48) |
H | 0.142/−0.1 | −0.264/0.163 | −0.216/0.149 | 0.866/0.6 | 0.573/0.022 | −0.259/−0.047 | 8.8/7.4** | 3.42/3.43 |
MH | 0.116/−0.081 | 0.025/0.189 | −0.12/0.129 | 0.863/0.67 | 0.496/0.022 | −0.284/−0.046 | 19.1/10.7** | 3.42/3.43 |
ML | 0.128/−0.025 | 0.018/0.156 | −0.121/0.097 | 0.761/0.608 | 0.315/0.004 | −0.19/−0.071 | 10.2/7.3** | 3.42/3.43 |
L | 0.328/−0.115 | −0.278/0.12 | −0.227/0.163 | 0.917/0.626 | 0.351/0.081 | −0.309/−0.045 | 8.9/9.3** | 3.42/3.43 |
All | 0.199/−0.09 | −0.148/0.16 | −0.181/0.141 | 0.901/0.638 | 0.461/0.037 | −0.287/−0.049 | 11.8/9.2** | 3.42/3.43 |
The response surface was defined by a quadratic surface function: .
Here, Z = Z score value of standardized tree ring index at different elevations and the whole site; X = Z score value of mean precipitation (previous July to current June); Y = Z score value of mean temperature (previous September to current March). The F value is calculated by , with notation as follows. : regression sum of squares, : residual sum of squares, p: degrees of freedom of the regression function, here p = 5, n: number of active data, here n = 55. If , the response surface regression is significant at the α level.
F value is significant at p = 0.01 level.