Table 1 Results of the linear mixed-effect models (LME).
From: Carbon dioxide fluxes increase from day to night across European streams
Response variable | Fixed effect | χ2 (1) | p | Sign | |
|---|---|---|---|---|---|
(A) Testing spatial and temporal hypotheses | |||||
CO2 flux difference from day to night | Latitude | 7.4207 | 0.006 | − | |
Water temperature (day) | 0.0168 | 0.897 | |||
Water temperature (day)*latitude | 4.9594 | 0.026 | + | ||
(B) Testing physical and biogeochemical drivers of CO2 flux changes | |||||
CO2 flux difference from day to night | Δ Water pCO2 | 4.9497 | 0.026 | + | |
Δ Gas transfer velocity k | 0.5613 | 0.454 | |||
(C) Testing biogeochemical drivers of pCO2 changes | |||||
pCO2 difference from day to night | Δ Water O2 concentration | 7.9879 | 0.005 | − | |
ΔpH | 0.0345 | 0.853 | |||
Δ Conductivity | 0.0293 | 0.864 | |||
ΔTw−Ta a (proxy for heat flux) | 1.6720 | 0.196 | |||
ΔWater temperature | 0.8731 | 0.350 | |||
(D) Testing catchment and hydromorphological drivers of pCO2 changes | |||||
pCO2 difference from day to night | Day length | 1.7244 | 0.189 | ||
Stream wetted width | 0.3748 | 0.540 | |||
Discharge | 3.4458 | 0.063 | |||
% forest | 0.0950 | 0.758 | |||
Catchment area | 2.3656 | 0.124 | |||