Show simple item record

dc.contributor.authorZhou, S
dc.contributor.authorLiang, J
dc.contributor.authorLuc, X
dc.contributor.authorLid, Q
dc.contributor.authorJiang, L
dc.contributor.authorZhang, Y
dc.contributor.authorSchwalm, CR
dc.contributor.authorFisher, JB
dc.contributor.authorTjiputra, J
dc.contributor.authorSitch, S
dc.contributor.authorAhlström, A
dc.contributor.authorHuntzinger, DN
dc.contributor.authorHuang, Y
dc.contributor.authorWang, G
dc.contributor.authorLuo, Y
dc.date.accessioned2018-10-24T13:20:54Z
dc.date.issued2018-03-12
dc.description.abstractTerrestrial carbon cycle models have incorporated increasingly more processes as a means to achieve more-realistic representations of ecosystem carbon cycling. Despite this, there are large across-model variations in the simulation and projection of carbon cycling. Several model intercomparison projects (MIPs), for example, the fifth phase of the Coupled Model Intercomparison Project (CMIP5) (historical simulations), Trends in Net Land-Atmosphere Carbon Exchange (TRENDY), and Multiscale Synthesis and Terrestrial Model Intercomparison Project (MsTMIP), have sought to understand intermodel differences. In this study, the authors developed a suite of new techniques to conduct post-MIP analysis to gain insights into uncertainty sources across 25 models in the three MIPs. First, terrestrial carbon storage dynamics were characterized by a three-dimensional (3D) model output space with coordinates of carbon residence time, net primary productivity (NPP), and carbon storage potential. The latter represents the potential of an ecosystem to lose or gain carbon. This space can be used to measure how and why model output differs. Models with a nitrogen cycle generally exhibit lower annual NPP in comparison with other models, and mostly negative carbon storage potential. Second, a transient traceability framework was used to decompose any given carbon cycle model into traceable components and identify the sources of model differences. The carbon residence time (or NPP) was traced to baseline carbon residence time (or baseline NPP related to the maximum carbon input), environmental scalars, and climate forcing. Third, by applying a variance decomposition method, the authors show that the intermodel differences in carbon storage can be mainly attributed to the baseline carbon residence time and baseline NPP (>90% in the three MIPs). The three techniques developed in this study offer a novel approach to gain more insight from existing MIPs and can point out directions for future MIPs. Since this study is conducted at the global scale for an overview on intermodel differences, future studies should focus more on regional analysis to identify the sources of uncertainties and improve models at the specified mechanism level.en_GB
dc.description.sponsorshipThis paper is financially supported by the Research and Development Special Fund for Public Welfare Industry of the Ministry of Water Research in China (201501028). JBF and CRS were supported in part by NASA’s Carbon Cycle Science program. JBF was also supported in part by NASA’s Terrestrial Ecology and Carbon Monitoring System programs. JT acknowledges RCN funded project EVA (229771) and BCCR-BIGCHANGE.en_GB
dc.identifier.citationVol. 31 (7), pp. 2833 - 2851en_GB
dc.identifier.doi10.1175/JCLI-D-17-0357.1
dc.identifier.urihttp://hdl.handle.net/10871/34419
dc.language.isoenen_GB
dc.publisherAmerican Meteorological Societyen_GB
dc.rights© 2018 American Meteorological Society.en_GB
dc.subjectCarbon cycleen_GB
dc.subjectLand surface modelen_GB
dc.subjectModel evaluation/performanceen_GB
dc.titleSources of uncertainty in modeled land carbon storage within and across three MIPs: Diagnosis with three new techniquesen_GB
dc.typeArticleen_GB
dc.date.available2018-10-24T13:20:54Z
dc.identifier.issn0894-8755
dc.descriptionThis is the final version. Available from the American Meteorological Society via the DOI in this recorden_GB
dc.identifier.journalJournal of Climateen_GB


Files in this item

This item appears in the following Collection(s)

Show simple item record