Analysing Amazonian forest productivity using a new individual and trait-based model (TFS v.1)
Authored by N M Fyllas, E Gloor, L M Mercado, S Sitch, C A Quesada, T F Domingues, D R Galbraith, A Torre-Lezama, E Vilanova, H Ramirez-Angulo, N Higuchi, D A Neill, M Silveira, L Ferreira, C G A Aymard, Y Malhi, O L Phillips, J Lloyd
Date Published: 2014
DOI: 10.5194/gmd-7-1251-2014
Sponsors:
European Union
United Kingdom Natural Environment Research Council (NERC)
Platforms:
Java
Model Documentation:
Other Narrative
Mathematical description
Model Code URLs:
Model code not found
Abstract
Repeated long-term censuses have revealed large-scale spatial patterns
in Amazon basin forest structure and dynamism, with some forests in the
west of the basin having up to a twice as high rate of aboveground
biomass production and tree recruitment as forests in the east. Possible
causes for this variation could be the climatic and edaphic gradients
across the basin and/or the spatial distribution of tree species
composition. To help understand causes of this variation a new
individual-based model of tropical forest growth, designed to take full
advantage of the forest census data available from the Amazonian Forest
Inventory Network (RAIN-FOR), has been developed. The model allows for
within-stand variations in tree size distribution and key functional
traits and between-stand differences in climate and soil physical and
chemical properties. It runs at the stand level with four functional
traits - leaf dry mass per area (M-a), leaf nitrogen (N-L) and
phosphorus (P-L) content and wood density (D-W) varying from tree to
tree - in a way that replicates the observed continua found within each
stand. We first applied the model to validate canopy-level water fluxes
at three eddy covariance flux measurement sites. For all three sites the
canopy-level water fluxes were adequately simulated. We then applied the
model at seven plots, where intensive measurements of carbon allocation
are available. Tree-by-tree multi-annual growth rates generally agreed
well with observations for small trees, but with deviations identified
for larger trees. At the stand level, simulations at 40 plots were used
to explore the influence of climate and soil nutrient availability on
the gross (Pi(G)) and net (Pi(N)) primary production rates as well as
the carbon use efficiency (C-U). Simulated Pi(G), Pi(N) and C-U were not
associated with temperature. On the other hand, all three measures of
stand level productivity were positively related to both mean annual
precipitation and soil nutrient status. Sensitivity studies showed a
clear importance of an accurate parameterisation of within- and
between-stand trait variability on the fidelity of model predictions.
For example, when functional tree diversity was not included in the
model (i.e. with just a single plant functional type with mean
basin-wide trait values) the predictive ability of the model was
reduced. This was also the case when basin-wide (as opposed to
site-specific) trait distributions were applied within each stand. We
conclude that models of tropical forest carbon, energy and water cycling
should strive to accurately represent observed variations in
functionally important traits across the range of relevant scales.
Tags
net primary productivity
Climate-change
Tropical rain-forests
Carbon allocation
Woody-tissue
respiration
Global vegetation models
Basin-wide variations
Long-term
plots
Functional composition
Economics spectrum