The sensitivity of stand-scale photosynthesis and transpiration to changes in atmospheric CO2 concentration and climate

Fig- ure 3 shows surface reaching DCP, vertical structure of DCP production rate, updraft mass flux, and cloud liquid water.. Figure 3a3 shows that updraft mass flux in TAU (1 h)

There was no influence of elevated [CO2] on copy numbers of archaeal or bacterial 16S rRNA or amo A genes, archaeal community composition, KCl-extractable soil ammonium or nitrite,

Moreover, we assessed how these numbers changed through time given the changing socioeconomic conditions, relative to developments in (1) the population and land area sensitive

Using four different climate models, we investi- gate sea level pressure variability in the extratropical North Atlantic in the preindustrial climate (1750 AD) and at the Last

doi:10.1371/journal.pcbi.1003195.g004.. Thus, the shadow prices associated with individual intracellular metabolites provide information not only about the extent to which

Within-canopy heterogeneous light conditions were the most important contribution to the within-canopy heterogeneity of the simulated photosynthesis and transpiration rates. 4) showed

Specific objectives were to: (1) test the general validity of a model simulating the seasonal patterns of carbon, wa- ter and heat fluxes of a Norway spruce stand at Knott˚asen,

As a consequence, the ratio of deposition velocities (uptake rate divided by ambient mole fraction) for leaf COS and CO 2 fluxes can provide an estimate of C i /C a , the ratio