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Nitrogen Availability Dampens the Positive Impacts of CO 2 Fertilization on Terrestrial Ecosystem Carbon and Water Cycles
Author(s) -
He Liming,
Chen Jing M.,
Croft Holly,
Gonsamo Alemu,
Luo Xiangzhong,
Liu Jane,
Zheng Ting,
Liu Ronggao,
Liu Yang
Publication year - 2017
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2017gl075981
Subject(s) - environmental science , evapotranspiration , water use efficiency , primary production , ecosystem , photosynthesis , terrestrial ecosystem , carbon sink , carbon cycle , atmospheric sciences , stomatal conductance , water cycle , agronomy , fluxnet , ecology , eddy covariance , botany , biology , geology
Abstract The magnitude and variability of the terrestrial CO 2 sink remain uncertain, partly due to limited global information on ecosystem nitrogen (N) and its cycle. Without N constraint in ecosystem models, the simulated benefits from CO 2 fertilization and CO 2 ‐induced increases in water use efficiency (WUE) may be overestimated. In this study, satellite observations of a relative measure of chlorophyll content are used as a proxy for leaf photosynthetic N content globally for 2003–2011. Global gross primary productivity (GPP) and evapotranspiration are estimated under elevated CO 2 and N‐constrained model scenarios. Results suggest that the rate of global GPP increase is overestimated by 85% during 2000–2015 without N limitation. This limitation is found to occur in many tropical and boreal forests, where a negative leaf N trend indicates a reduction in photosynthetic capacity, thereby suppressing the positive vegetation response to enhanced CO 2 fertilization. Based on our carbon‐water coupled simulations, enhanced CO 2 concentration decreased stomatal conductance and hence increased WUE by 10% globally over the 1982 to 2015 time frame. Due to increased anthropogenic N application, GPP in croplands continues to grow and offset the weak negative trend in forests due to N limitation. Our results also show that the improved WUE is unlikely to ease regional droughts in croplands because of increases in evapotranspiration, which are associated with the enhanced GPP. Although the N limitation on GPP increase is large, its associated confidence interval is still wide, suggesting an urgent need for better understanding and quantification of N limitation from satellite observations.