Ss-scale modelling, by explicitly such as individual stomata. The findings on the

Inside the BUdR site present study, however, the surface concentration in the sources was taken to become continuous (see `Boundary conditions for air flow').Ss-scale modelling, by explicitly including individual stomata. The white location indicates the leaf surface.Ss-scale modelling, by explicitly including person stomata. The findings from the present study can very easily beDefraeye et al. -- Cross-scale modelling of stomatal transpiration through the boundary layerFLO WFLOWxv,iso = 0?08950 kgv kg? Iv = 70Coverage ratio 0?5 xv,iso = 0?05673 kgv kg? Iv = 8FLO WFLO Wxv,iso = 0?06836 kgv kg? Iv = 30Coverage ratio 1 xv,iso = 0?06836 kgv kg? Iv = 30FLO WFLO WCoverage ratio five xv,iso = 0?08950 kgv kg? Iv = 70 xv,iso = 0?06572 kgv kg? Iv = 25FLO WFLO WCoverage ratio 10 xv,iso = 0?09742 kgv kg? Iv = 85 xv,iso = 0?06308 kgv kg? Iv = 20 0 m s? 2?3 m s? 0 m s? 2?three m s?F I G . 9. Typical water vapour concentration isocontours (i.e. of continual xv) in the boundary layer above the leaf surface for Ub ?two m s21 at a CR of 1 . The dimensionless isocontour value (Iv) is also provided. These isocontours are coloured as outlined by air speed. A single isocontour is shown per image. Additionally, air speeds in a horizontal and vertical centreplane are also shown. The cross-section between these planes is indicated by the black line. The white area indicates the leaf surface. SART.S23503 The colour scale consists of the complete air speed variety.F I G . ten. Water vapour concentration isocontours (i.e. of continuous xv) in the boundary layer above the leaf surface for Ub ?two m s21 at different CRs (0.25, 1, 5 and 10 ). The dimensionless isocontour value (IV) can also be given. These isocontours are coloured in line with air speed. 1 isocontour is shown per image. Additionally, air speeds in a horizontal and vertical centreplane are also shown. The cross-section among these planes is indicated by the black line. The white area indicates the leaf surface. The colour scale includes the whole air speed variety.transferred to BLCs of other scalars, such geronb/gbp074 as CO2, but also to evaporation of microscopic droplets on leaf surfaces (see Defraeye et al., 2013a).Defraeye et al. -- Cross-scale modelling of stomatal transpiration by way of the boundary layer The developed numerical model permits us to study the transport mechanisms involved, but is still simplified in some elements (e.g. a flat, smooth leaf surface). Future model developments are briefly listed under. (1) Convective transfer in the boundary layer was not coupled to transport inside the leaf, i.e. in the mesophyll cells (RH 100 ) by means of the intercellular spaces through the stomata towards the leaf surface. To quantify the actual transpiration rate, these resistances ought to also be accounted for in the model. Furthermore, this would permit us also to assess boundary-layer interference involving stomata, i.e. the impact of stomatal transpiration around the concentration in the surface with the stomata additional downstream (Cannon et al., 1979). In the present study, nonetheless, the surface concentration in the sources was taken to become continual (see `Boundary conditions for air flow').