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Estimating parameters in a land‐surface model by applying nonlinear inversion to eddy covariance flux measurements from eight FLUXNET sites
Author(s) -
WANG YING PING,
BALDOCCHI DENNIS,
LEUNING RAY,
FALGE EVA,
VESALA TIMO
Publication year - 2007
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/j.1365-2486.2006.01225.x
Subject(s) - fluxnet , eddy covariance , evergreen , atmospheric sciences , biometeorology , environmental science , biosphere model , leaf area index , deciduous , sensible heat , canopy , biosphere , ecosystem , ecology , biology , geology
Flux measurements from eight global FLUXNET sites were used to estimate parameters in a process‐based, land‐surface model (CSIRO Biosphere Model (CBM), using nonlinear parameter estimation techniques. The parameters examined were the maximum photosynthetic carboxylation rate () the potential photosynthetic electron transport rate ( j max, 25 ) of the leaf at the top of the canopy, and basal soil respiration ( r s, 25 ), all at a reference temperature of 25°C. Eddy covariance measurements used in the analysis were from four evergreen forests, three deciduous forests and an oak‐grass savanna. Optimal estimates of model parameters were obtained by minimizing the weighted differences between the observed and predicted flux densities of latent heat, sensible heat and net ecosystem CO 2 exchange for each year. Values of maximum carboxylation rates obtained from the flux measurements were in good agreement with independent estimates from leaf gas exchange measurements at all evergreen forest sites. A seasonally varying and j max, 25 in CBM yielded better predictions of net ecosystem CO 2 exchange than a constant and j max, 25 for all three deciduous forests and one savanna site. Differences in the seasonal variation of and j max, 25 among the three deciduous forests are related to leaf phenology. At the tree‐grass savanna site, seasonal variation of and j max, 25 was affected by interactions between soil water and temperature, resulting in and j max, 25 reaching maximal values before the onset of summer drought at canopy scale. Optimizing the photosynthetic parameters in the model allowed CBM to predict quite well the fluxes of water vapor and CO 2 but sensible heat fluxes were systematically underestimated by up to 75 W m −2 .

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