@article{
 title = {Linking flux network measurements to continental scale simulations: Ecosystem carbon dioxide exchange capacity under non-water-stressed conditions},
 type = {article},
 year = {2007},
 keywords = {Carbon dioxide exchange,Crops,Eddy covariance,Forest,Grassland,Gross primary production,Model inversion,Net ecosystem exchange,Up-scaling,Wetland},
 pages = {734-760},
 volume = {13},
 id = {d563bb78-77f6-3b60-bd98-84e071a275a5},
 created = {2018-01-18T16:53:31.490Z},
 file_attached = {false},
 profile_id = {5c1040db-25e3-36ea-a919-0994a44709e7},
 group_id = {c4af41cc-7e3c-3fd3-9982-bdb923596eee},
 last_modified = {2020-09-08T15:25:47.868Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Owen2007},
 private_publication = {false},
 abstract = {This paper examines long-term eddy covariance data from 18 European and 17 North American and Asian forest, wetland, tundra, grassland, and cropland sites under non-water-stressed conditions with an empirical rectangular hyperbolic light response model and a single layer two light-class carboxylase-based model. Relationships according to ecosystem functional type are demonstrated between empirical and physiological parameters, suggesting linkages between easily estimated parameters and those with greater potential for process interpretation. Relatively sparse documentation of leaf area index dynamics at flux tower sites is found to be a major difficulty in model inversion and flux interpretation. Therefore, a simplification of the physiological model is carried out for a subset of European network sites with extensive ancillary data. The results from these selected sites are used to derive a new parameter and means for comparing empirical and physiologically based methods across all sites, regardless of ancillary data. The results from the European analysis are then compared with results from the other Northern Hemisphere sites and similar relationships for the simplified process-based parameter were found to hold for European, North American, and Asian temperate and boreal climate zones. This parameter is useful for bridging between flux network observations and continental scale spatial simulations of vegetation/atmosphere carbon dioxide exchange.},
 bibtype = {article},
 author = {Owen, Katherine E. and Tenhunen, John and Reichstein, Markus and Wang, Quan and Falge, Eva and Geyer, Ralf and Xiao, Xiangming and Stoy, Paul C. and Ammann, Christof and Arain, Altaf and Aubinet, Marc and Aurela, Mika and Bernhofer, Christian and Chojnicki, Bogdan H. and Granier, André and Gruenwald, Thomas and Hadley, Julian and Heinesch, Bernard and Hollinger, David and Knohl, Alexander and Kutsch, Werner and Lohila, Annalea and Meyers, Tilden and Moors, Eddy J. and Moureaux, Christine and Pilegaard, Kim and Saigusa, Nobuko and Verma, Shashi and Vesala, Timo and Vogel, Chris},
 doi = {10.1111/j.1365-2486.2007.01326.x},
 journal = {Global Change Biology},
 number = {4}
}

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