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The importance of micrometeorological variations for photosynthesis and transpiration in a boreal coniferous forest

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Figure

Figure 1. Relationship between the relative amount of incoming ra-diation at the surface (as a fraction of top-of-atmosphere radiation)ftrans and diffuse fraction fdif
Table 2. Overview of the simulations performed for this study.
Figure 3. Diurnal cycle of simulated and observed (a) CO2 assim-ilation and (b) transpiration, averaged for four seasons with datafrom 1999, 2000 and 2002.
Figure 4. Overview of vertical gradients in the canopy for three periods: 18–22 May 1999 (case 1), 24–28 August 1999 (case 2) and 8–12Gradients in COinSeptember 1999 (case 3)
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