Metadata Field | Value | Language |
dc.contributor | Hanqin Tian, [email protected] | en_US |
dc.creator | Luo, Yiqi | |
dc.creator | Ahlstrom, Anders | |
dc.creator | Allison, Steven D. | |
dc.creator | Batjes, Niles H. | |
dc.creator | Brovkin, Victor | |
dc.creator | Carvalhais, Nuno | |
dc.creator | Chappell, Adrian | |
dc.creator | Ciais, Philippe | |
dc.creator | Davidson, Eric A. | |
dc.creator | Finzi, Adrien C. | |
dc.creator | Georgiou, Katerina | |
dc.creator | Guenet, Bertrand | |
dc.creator | Hararuk, Oleksandra | |
dc.creator | Harden, Jennifer W. | |
dc.creator | He, Yujie | |
dc.creator | Hopkins, Francesca | |
dc.creator | Jiang, Lifen | |
dc.creator | Koven, Charlie | |
dc.creator | Jackson, Robert B. | |
dc.creator | Jones, Chris D. | |
dc.creator | Lara, Mark J. | |
dc.creator | Liang, Junyi | |
dc.creator | McGuire, A. David | |
dc.creator | Parton, William | |
dc.creator | Peng, Changhui | |
dc.creator | Randerson, James T. | |
dc.creator | Salazar, Alejandro | |
dc.creator | Sierra, Carlos A. | |
dc.creator | Smith, Mathew J. | |
dc.creator | Tian, Hanqin | |
dc.creator | Todd-Brown, Katherine E.O. | |
dc.creator | Torn, Margaret | |
dc.creator | van Groenigen, Kees Jan | |
dc.creator | Wang, Ying Ping | |
dc.creator | West, Tristram O. | |
dc.creator | Wei, Yaxing | |
dc.creator | Wieder, William R | |
dc.creator | Xia, Jianyang | |
dc.creator | Xu, Xia | |
dc.creator | Xu, Xiaofeng | |
dc.creator | Zhou, Tao | |
dc.date.accessioned | 2022-03-03T16:06:30Z | |
dc.date.available | 2022-03-03T16:06:30Z | |
dc.date.created | 2016-01 | |
dc.identifier | 10.1002/2015GB005239 | en_US |
dc.identifier.uri | https://agupubs-onlinelibrary-wiley-com.spot.lib.auburn.edu/doi/full/10.1002/2015GB005239 | en_US |
dc.identifier.uri | https://aurora.auburn.edu/handle/11200/50030 | |
dc.identifier.uri | http://dx.doi.org/10.35099/aurora-99 | |
dc.description.abstract | Soil carbon (C) is a critical component of Earth system models (ESMs), and its diverse representations are a major source of the large spread across models in the terrestrial C sink from the third to fifth assessment reports of the Intergovernmental Panel on Climate Change (IPCC). Improving soil C projections is of a high priority for Earth system modeling in the future IPCC and other assessments. To achieve this goal, we suggest that (1) model structures should reflect real-world processes, (2) parameters should be calibrated to match model outputs with observations, and (3) external forcing variables should accurately prescribe the environmental conditions that soils experience. First, most soil C cycle models simulate C input from litter production and C release through decomposition. The latter process has traditionally been represented by first-order decay functions, regulated primarily by temperature, moisture, litter quality, and soil texture. While this formulation well captures macroscopic soil organic C (SOC) dynamics, better understanding is needed of their underlying mechanisms as related to microbial processes, depth-dependent environmental controls, and other processes that strongly affect soil C dynamics. Second, incomplete use of observations in model parameterization is a major cause of bias in soil C projections from ESMs. Optimal parameter calibration with both pool-and flux-based data sets through data assimilation is among the highest priorities for near-term research to reduce biases among ESMs. Third, external variables are represented inconsistently among ESMs, leading to differences in modeled soil C dynamics. We recommend the implementation of traceability analyses to identify how external variables and model parameterizations influence SOC dynamics in different ESMs. Overall, projections of the terrestrial C sink can be substantially improved when reliable data sets are available to select the most representative model structure, constrain parameters, and prescribe forcing fields. | en_US |
dc.format | PDF | en_US |
dc.publisher | AMER GEOPHYSICAL UNION | en_US |
dc.relation.ispartof | GLOBAL BIOGEOCHEMICAL CYCLES | en_US |
dc.relation.ispartofseries | 0886-6236 | en_US |
dc.rights | ©American Geophysical Union 2016. This is this the version of record co-published by the American Geophysical Union and John Wiley & Sons, Inc. It is made available under the CC-BY-NC-ND 4.0 license. Item should be cited as: Luo, Y., Ahlström, A., Allison, S. D., Batjes, N. H., Brovkin, V., Carvalhais, N., ... & Zhou, T. (2016). Toward more realistic projections of soil carbon dynamics by Earth system models. Global Biogeochemical Cycles, 30(1), 40-56. | en_US |
dc.subject | GLOBAL CLIMATE-CHANGE | en_US |
dc.subject | ORGANIC-CARBON | en_US |
dc.subject | DATA-ASSIMILATION | en_US |
dc.subject | HETEROTROPHIC RESPIRATION | en_US |
dc.subject | TEMPERATURE SENSITIVITY | en_US |
dc.subject | TERRESTRIAL ECOSYSTEMS | en_US |
dc.subject | LITTER DECOMPOSITION | en_US |
dc.subject | PARAMETER-ESTIMATION | en_US |
dc.subject | MICROBIAL MODELS | en_US |
dc.subject | LAND MODELS | en_US |
dc.title | Toward more realistic projections of soil carbon dynamics by Earth system models | en_US |
dc.type | Text | en_US |
dc.type.genre | Journal Article, Academic Journal | en_US |
dc.citation.volume | 30 | en_US |
dc.citation.issue | 1 | en_US |
dc.citation.spage | 40 | en_US |
dc.citation.epage | 56 | en_US |
dc.description.status | Published | en_US |
dc.description.peerreview | Yes | en_US |
dc.creator.orcid | 0000-0002-1806-4091 | en_US |
dc.contributor.department | School of Forestry and Wildlife Sciences | en_US |