Although similar interactions are observed between both size-frequency distribution estimates (gradient and intercept), the interaction between WSG and maximum canopy height is inverse, with carbon storage only showing positive correlations with maximum canopy height in areas of high WSG.
After they reached their maximum heights, the biomass and carbon storage were determined.
With these simple treatments and assumptions to link the woody carbon storage with the maximum LAI, we modeled phenological processes of deciduous L. kaempferi.
Our estimate of peat carbon storage exceeds the 21.6 GtC maximum estimated carbon stock in above- and belowground biomass of all Indonesian forests by 30%[51]], an observation similarly noted by Dommain et al. [9].
(DOC 254 KB) 13021_2013_99_MOESM6_ESM.doc Additional file 6: Figure S5: The 2nd order interactions relating my carbon storage derivatives (wood specific gravity, maximum canopy height, the intercept of the power law relationship, and the gradient of the power law relationship [shown here as WSG, height, intercept, and gradient respectively]) to aboveground live carbon storage.
Considering only second order interactions, in areas of low potential stem density, carbon storage is positively correlated with maximum canopy height (Additional file 6: Figure S5).
I measured the heights of bamboo culms in different diameter classes daily, and then these bamboos were felled to determine their biomass and to estimate the carbon storage capacity after the culms reached maximum height.
Using the production approach, a nationwide maximum figure of 2.9 MtC year−1 for the HWP carbon storage effect is determined for 2030.
Because obtaining the maximum potential area of Holocene natural (pre-settlement) wetlands and carbon storage was our objective, the 2011 wetland map was used to adjust the DUC's pre-settlement map.
