TY - JOUR
T1 - Effects of model structural uncertainty on carbon cycle projections
T2 - Biological nitrogen fixation as a case study
AU - Wieder, William R.
AU - Cleveland, Cory C.
AU - Lawrence, David M.
AU - Bonan, Gordon B.
N1 - Publisher Copyright:
© 2015 IOP Publishing Ltd.
PY - 2015/4/1
Y1 - 2015/4/1
N2 - Uncertainties in terrestrial carbon (C) cycle projections increase uncertainty of potential climate feedbacks. Efforts to improve model performance often include increased representation of biogeochemical processes, such as coupled carbon-nitrogen (N) cycles. In doing so, models are becoming more complex, generating structural uncertainties in model form that reflect incomplete knowledge of how to represent underlying processes. Here, we explore structural uncertainties associated with biological nitrogen fixation (BNF) and quantify their effects on C cycle projections. We find that alternative plausible structures to represent BNF result in nearly equivalent terrestrial C fluxes and pools through the twentieth century, but the strength of the terrestrial C sink varies by nearly a third (50 Pg C) by the end of the twenty-first century under a business-as-usual climate change scenario representative concentration pathway 8.5. These results indicate that actual uncertainty in future C cycle projections may be larger than previously estimated, and this uncertainty will limit C cycle projections until model structures can be evaluated and refined.
AB - Uncertainties in terrestrial carbon (C) cycle projections increase uncertainty of potential climate feedbacks. Efforts to improve model performance often include increased representation of biogeochemical processes, such as coupled carbon-nitrogen (N) cycles. In doing so, models are becoming more complex, generating structural uncertainties in model form that reflect incomplete knowledge of how to represent underlying processes. Here, we explore structural uncertainties associated with biological nitrogen fixation (BNF) and quantify their effects on C cycle projections. We find that alternative plausible structures to represent BNF result in nearly equivalent terrestrial C fluxes and pools through the twentieth century, but the strength of the terrestrial C sink varies by nearly a third (50 Pg C) by the end of the twenty-first century under a business-as-usual climate change scenario representative concentration pathway 8.5. These results indicate that actual uncertainty in future C cycle projections may be larger than previously estimated, and this uncertainty will limit C cycle projections until model structures can be evaluated and refined.
KW - Earth system modeling
KW - biological nitrogen fixation
KW - carbon cycle
KW - climate change
KW - community land model
KW - structural uncertainty
UR - http://www.scopus.com/inward/record.url?scp=84928717828&partnerID=8YFLogxK
U2 - 10.1088/1748-9326/10/4/044016
DO - 10.1088/1748-9326/10/4/044016
M3 - Article
AN - SCOPUS:84928717828
SN - 1748-9318
VL - 10
JO - Environmental Research Letters
JF - Environmental Research Letters
IS - 4
M1 - 044016
ER -