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. 2020 Oct 19;8:e10113. doi: 10.7717/peerj.10113

Table 3. Approximate significance of smooth terms in Shaanbei upland plateau and Guanzhong basin in Shaanxi Province, China, 2005–2018.

Variables Regions Effective degrees of freedom F p
s(Air temperature) Guanzhong basin 6.41 1.80 0.08
Shaanbei upland plateau 1.00 0.86 0.35
s(Lag in air temperature) Guanzhong basin 7.73 1.49 0.15
Shaanbei upland plateau 1.59 4.34 0.01
s(Relative humidity) Guanzhong basin 5.44 3.61 <0.001
Shaanbei upland plateau 1.00 0.12 0.73
s(Lag in relative humidity) Guanzhong basin 6.62 4.06 <0.001
Shaanbei upland plateau 1.00 4.21 0.04
s(Sunshine duration) Guanzhong basin 2.37 2.71 0.04
Shaanbei upland plateau 1.75 3.18 0.04
s(Lag in sunshine duration) Guanzhong basin 9.41 1.66 0.09
Shaanbei upland plateau 1.00 4.64 0.03
s(Evaporation) Guanzhong basin 3.47 4.60 <0.001
Shaanbei upland plateau 2.31 1.63 0.21
s(Lag in evaporation) Guanzhong basin 1.30 6.37 0.01
Shaanbei upland plateau 1.00 4.01 0.05
s(Rainfall) Guanzhong basin 8.61 2.38 0.01
Shaanbei upland plateau 1.00 0.12 0.73
s(Lag in rainfall) Guanzhong basin 8.23 1.75 0.08
Shaanbei upland plateau 1.00 0.42 0.52

Notes.

*

Summary of the GAMM smooth terms, their p-values and effective degrees of freedom are listed. We constructed the final model based on current monthly meteorological factors, temperature lag of 4 months, rainfall lag of 3 months, relative humidity lag of 2 months, sunshine duration lag of 6 months and evaporation lag of 5 months in Shaanbei upland plateau. Meanwhile, we constructed the final model for the Guanzhong basin based on current monthly meteorological factors and previous meteorological factors with lag times 1 month greater than those in Shaanbei upland plateau.