Hydrology and Land Surface Studies
Terrestrial nitrogen feedbacks may accelerate future climate change
Version of Record online: 5 JAN 2010
Copyright 2010 by the American Geophysical Union.
Geophysical Research Letters
Volume 37, Issue 1, January 2010
How to Cite
2010), Terrestrial nitrogen feedbacks may accelerate future climate change, Geophys. Res. Lett., 37, L01401, doi:10.1029/2009GL041345., , and (
- Issue online: 5 JAN 2010
- Version of Record online: 5 JAN 2010
- Manuscript Accepted: 10 DEC 2009
- Manuscript Revised: 25 NOV 2009
- Manuscript Received: 13 OCT 2009
Auxiliary material for this article contains the exact protocol and forcing data used to make O-C and O-CN model runs, a text describing the auxliary model results, key characteristics of the simulated 2000 C stocks and fluxes in O-C and O-CN, and figures in support of Figures 1, 2, and 3.
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Additional file information is provided in the readme.txt.
|grl26634-sup-0001-readme.txt||plain text document||4K||readme.txt|
|grl26634-sup-0002-txts01.tex||application/x-tex||999||Text S1. Description of the initialization procedure of the model, as well as all the forcing data sets used to perform simulations.|
|grl26634-sup-0003-txts01.pdf||PDF document||69K||Text S1. Description of the initialization procedure of the model, as well as all the forcing data sets used to perform simulations.|
|grl26634-sup-0004-txts02.tex||application/x-tex||999||Text S2. Description of the auxiliary model results.|
|grl26634-sup-0005-txts02.pdf||PDF document||67K||Text S2. Description of the auxiliary model results.|
|grl26634-sup-0006-ts01.tex||application/x-tex||999||Table S1. Key characteristics of the global C cycle simulated by O-C and O-CN.|
|grl26634-sup-0007-ts01.pdf||PDF document||34K||Table S1. Key characteristics of the global C cycle simulated by O-C and O-CN.|
|grl26634-sup-0008-fs01.eps||PS document||4K||Figure S1. Response of net primary production at the Duke Forest FACE experiment to 4 years of fertilizer application and elevated CO2.|
|grl26634-sup-0009-fs02.eps||PS document||8K||Figure S2. Observed and modeled effects of 10 years of 5°C soil warming in Harvard Forest on soil, vegetation, and total ecosystem carbon stocks.|
|grl26634-sup-0010-fs03.jpg||image/pjpeg||689K||Figure S3. Modeled responses of mean annual net primary production to 5 years of elevated CO2 and increased soil temperatures.|
|grl26634-sup-0011-fs04.jpg||image/pjpeg||1165K||Figure S4. Changes in terrestrial C storage [kg C m−2] between 1860 and 2071–2100 due to transient increases in atmospheric [CO2], transient climate change, and all transient factors combined for O-C and O-CN.|
|grl26634-sup-0012-fs05.eps||PS document||21K||Figure S5. Effect of the synergism between forcing factors CO2, CLIM, and NDEP on the derived land carbon CO2 sensitivity and climate sensitivity for O-CN and O-C.|
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