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Nitrogen attenuation of terrestrial carbon cycle response to global environmental factors
Author(s) -
Jain Atul,
Yang Xiaojuan,
Kheshgi Haroon,
McGuire A. David,
Post Wilfred,
Kicklighter David
Publication year - 2009
Publication title -
global biogeochemical cycles
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.512
H-Index - 187
eISSN - 1944-9224
pISSN - 0886-6236
DOI - 10.1029/2009gb003519
Subject(s) - carbon cycle , environmental science , carbon sink , nitrogen , sink (geography) , nitrogen cycle , carbon fibers , biogeochemical cycle , terrestrial ecosystem , carbon sequestration , atmospheric sciences , climate change , environmental chemistry , ecosystem , ecology , chemistry , geology , biology , geography , cartography , organic chemistry , composite number , materials science , composite material
Nitrogen cycle dynamics have the capacity to attenuate the magnitude of global terrestrial carbon sinks and sources driven by CO 2 fertilization and changes in climate. In this study, two versions of the terrestrial carbon and nitrogen cycle components of the Integrated Science Assessment Model (ISAM) are used to evaluate how variation in nitrogen availability influences terrestrial carbon sinks and sources in response to changes over the 20th century in global environmental factors including atmospheric CO 2 concentration, nitrogen inputs, temperature, precipitation and land use. The two versions of ISAM vary in their treatment of nitrogen availability: ISAM‐NC has a terrestrial carbon cycle model coupled to a fully dynamic nitrogen cycle while ISAM‐C has an identical carbon cycle model but nitrogen availability is always in sufficient supply. Overall, the two versions of the model estimate approximately the same amount of global mean carbon uptake over the 20th century. However, comparisons of results of ISAM‐NC relative to ISAM‐C reveal that nitrogen dynamics: (1) reduced the 1990s carbon sink associated with increasing atmospheric CO 2 by 0.53 PgC yr −1 (1 Pg = 10 15 g), (2) reduced the 1990s carbon source associated with changes in temperature and precipitation of 0.34 PgC yr −1 in the 1990s, (3) an enhanced sink associated with nitrogen inputs by 0.26 PgC yr −1 , and (4) enhanced the 1990s carbon source associated with changes in land use by 0.08 PgC yr −1 in the 1990s. These effects of nitrogen limitation influenced the spatial distribution of the estimated exchange of CO 2 with greater sink activity in high latitudes associated with climate effects and a smaller sink of CO 2 in the southeastern United States caused by N limitation associated with both CO 2 fertilization and forest regrowth. These results indicate that the dynamics of nitrogen availability are important to consider in assessing the spatial distribution and temporal dynamics of terrestrial carbon sources and sinks.