Canopy skin temperature variations in relation to climate, soil temperature, and carbon flux at a ponderosa pine forest in central Oregon
摘要
•The variation of canopy temperature was explained well by climatic variables.•A strong positive relationship was found between canopy and soil temperatures.•A weak negative relationship appeared between canopy temperatures and soil water.•Canopy temperatures were significantly related to afternoon-hour carbon exchange.•Canopy temperatures were more weakly related to latent heat fluxes.