HR: 09:40h
AN: B41F-07 [Abstracts]
TI: Carbon Cycle Steady State Assumption Impacts in Biogeochemical Modeling Inverse Parameter Retrieval and Implications for Regional Net Ecosystem Fluxes Estimates
AU: * Carvalhais, N
EM: ncarvalhais@fct.unl.pt
AF: Departamento de Cíncias e Engenharia do Ambiente
Faculdade de Cíncias e Tecnologia
Universidade Nova de Lisboa, Quinta da Torre - Monte de Caparica, Caparica, 2829 - 516, Portugal
AU: Reichstein, M
EM: markus.reichstein@bgc-jena.mpg.de
AU: Seixas, J
EM: mjs@fct.unl.pt
AF: Departamento de Cíncias e Engenharia do Ambiente
Faculdade de Cíncias e Tecnologia
Universidade Nova de Lisboa, Quinta da Torre - Monte de Caparica, Caparica, 2829 - 516, Portugal
AU: Collatz, G J
EM: jcollatz@ltpmail.gsfc.nasa.gov
AU: Pereira, J S
EM: jspereira@isa.utl.pt
AU: Berbigier, P
EM: berbigie@bordeaux.inra.fr
AU: Carrara, A
EM: arnaud@ceam.es
AU: Granier, A
EM: agranier@nancy.inra.fr
AU: Montagnani, L
EM: leonar@inwind.it
AU: Papale, D
EM: darpap@unitus.it
AU: Rambal, S
EM: serge.rambal@cefe.cnrs.fr
AU: Sanz, M J
EM: mjose@ceam.es
AU: Valentini, R
EM: rik@unitus.it
AB:
We analyze the impacts of the steady state assumption on inverse model parameter retrieval from
biogeochemical models. An inverse model parameterization study using eddy covariance CO2 flux data was
performed with the Carnegie Ames Stanford Approach (CASA) model under conditions of strict and relaxed
carbon-cycle steady state assumption (CCSSA), in order to evaluate both the robustness of the model’s
structure for the simulation of net ecosystem carbon fluxes and the assessment of the CCSSA effects on
simulations and parameter estimation. Net ecosystem production (NEP) measurements from several eddy-
covariance sites were compared with NEP estimates from the CASA model driven by local weather stations
climate inputs as well as by remotely sensed fraction of photosynthetically active radiation absorbed by vegetation
(fAPAR) and leaf area index (LAI). The parameters considered for optimization are directly related to above and
belowground modeled responses to temperature and water availability, as well as a parameter (η) that
relaxed the CCSSA in the model, allowing for site level simulations to be initialized either as net sinks or sources.
A robust relationship was observed between NEP observations and predictions for most of the sites through the
range of temporal scales considered (daily, weekly, biweekly and monthly), supporting the conclusion that the
model structure is able to capture the main processes explaining NEP variability. Overall, relaxing CCSSA
increased model efficiency and decreased normalized average error. Inter site variability was a major source of
variance in model performance differences between fix (CCSSAf) and relaxed (CCSSAr) CCSSA
conditions. These differences were correlated with mean annual NEP observations. A set of ancillary parameters
were tested as alternatives to η, yielding statistically significant lower model performance results. η was
found to be a key parameter in the optimization exercise, generating the highest model efficiency losses when
removed from the initial parameter set. Differences between ε* and Q10 estimates under
CCSSAr and CCSSAf conditions were correlated with η, suggesting parameter compensation effects
in steady state approaches. Parameter errors were significantly lower under CCSSAr. Overall, the importance
of model structure evaluation in data assimilation approaches is thus emphasized. Furthermore, using the
parameter estimates and their covariances we compute and analyze spatially distributed carbon balance
estimates for parts of Europe and associated uncertainties. Uncertainties introduced by wrong model
assumptions (e.g. CCSSA) clearly exceed the purely statistical uncertainties that come out of conventional data-
assimilation schemes.
DE: 0414 Biogeochemical cycles, processes, and modeling (0412, 0793, 1615, 4805, 4912)
DE: 0428 Carbon cycling (4806)
DE: 0466 Modeling
DE: 0480 Remote sensing
SC: Biogeosciences [B]
MN: 2007 Fall Meeting