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A model‐data comparison of gross primary productivity: Results from the North American Carbon Program site synthesis
Author(s) -
Schaefer Kevin,
Schwalm Christopher R.,
Williams Chris,
Arain M. Altaf,
Barr Alan,
Chen Jing M.,
Davis Kenneth J.,
Dimitrov Dimitre,
Hilton Timothy W.,
Hollinger David Y.,
Humphreys Elyn,
Poulter Benjamin,
Raczka Brett M.,
Richardson Andrew D.,
Sahoo Alok,
Thornton Peter,
Vargas Rodrigo,
Verbeeck Hans,
Anderson Ryan,
Baker Ian,
Black T. Andrew,
Bolstad Paul,
Chen Jiquan,
Curtis Peter S.,
Desai Ankur R.,
Dietze Michael,
Dragoni Danilo,
Gough Christopher,
Grant Robert F.,
Gu Lianhong,
Jain Atul,
Kucharik Chris,
Law Beverly,
Liu Shuguang,
Lokipitiya Erandathie,
Margolis Hank A.,
Matamala Roser,
McCaughey J. Harry,
Monson Russ,
Munger J. William,
Oechel Walter,
Peng Changhui,
Price David T.,
Ricciuto Dan,
Riley William J.,
Roulet Nigel,
Tian Hanqin,
Tonitto Christina,
Torn Margaret,
Weng Ensheng,
Zhou Xiaolu
Publication year - 2012
Publication title -
journal of geophysical research: biogeosciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2012jg001960
Subject(s) - primary production , eddy covariance , environmental science , atmospheric sciences , ecosystem respiration , biomass (ecology) , wind speed , canopy , ecosystem , carbon cycle , productivity , climatology , meteorology , ecology , geography , biology , geology , macroeconomics , economics
Accurately simulating gross primary productivity (GPP) in terrestrial ecosystem models is critical because errors in simulated GPP propagate through the model to introduce additional errors in simulated biomass and other fluxes. We evaluated simulated, daily average GPP from 26 models against estimated GPP at 39 eddy covariance flux tower sites across the United States and Canada. None of the models in this study match estimated GPP within observed uncertainty. On average, models overestimate GPP in winter, spring, and fall, and underestimate GPP in summer. Models overpredicted GPP under dry conditions and for temperatures below 0°C. Improvements in simulated soil moisture and ecosystem response to drought or humidity stress will improve simulated GPP under dry conditions. Adding a low‐temperature response to shut down GPP for temperatures below 0°C will reduce the positive bias in winter, spring, and fall and improve simulated phenology. The negative bias in summer and poor overall performance resulted from mismatches between simulated and observed light use efficiency (LUE). Improving simulated GPP requires better leaf‐to‐canopy scaling and better values of model parameters that control the maximum potential GPP, such as ε max (LUE), V cmax (unstressed Rubisco catalytic capacity) or J max (the maximum electron transport rate).

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