Comparison with Global Soil Radiocarbon Observations Indicates Needed Carbon Cycle Improvements in the E3SM Land Model

TitleComparison with Global Soil Radiocarbon Observations Indicates Needed Carbon Cycle Improvements in the E3SM Land Model
Publication TypeJournal Article
Year of Publication2019
JournalJournal of Geophysical Research: Biogeosciences
Number124
Date Published04/2019
Abstract / Summary

We evaluated global soil organic carbon (SOC) stocks and turnover time predictions from a global land model (ELMv1‐ECA) integrated in an Earth System Model (E3SM) by comparing them with observed soil bulk and Δ14C values around the world. We analyzed observed and simulated SOC stocks and Δ14C values using machine‐learning methods at the ESM gridcell scale (~200 km). In gridcells with sufficient observations, the model provided reasonable estimates of soil carbon stocks across soil depth and Δ14C values near the surface but underestimated Δ14C at depth. Among many explanatory variables, soil albedo index, soil order, plant function type (PFT), air temperature, and SOC content were major factors affecting predicted SOC Δ14C values. The influences of soil albedo index, soil order, and air temperature were primarily important in the shallow subsurface (

URLhttp://dx.doi.org/10.1029/2018jg004795
DOI10.1029/2018jg004795
Journal: Journal of Geophysical Research: Biogeosciences
Year of Publication: 2019
Number: 124
Date Published: 04/2019

We evaluated global soil organic carbon (SOC) stocks and turnover time predictions from a global land model (ELMv1‐ECA) integrated in an Earth System Model (E3SM) by comparing them with observed soil bulk and Δ14C values around the world. We analyzed observed and simulated SOC stocks and Δ14C values using machine‐learning methods at the ESM gridcell scale (~200 km). In gridcells with sufficient observations, the model provided reasonable estimates of soil carbon stocks across soil depth and Δ14C values near the surface but underestimated Δ14C at depth. Among many explanatory variables, soil albedo index, soil order, plant function type (PFT), air temperature, and SOC content were major factors affecting predicted SOC Δ14C values. The influences of soil albedo index, soil order, and air temperature were primarily important in the shallow subsurface (

DOI: 10.1029/2018jg004795
Citation:
Chen, J, Q Zhu, W Riley, Y He, J Randerson, and S Trumbore.  2019.  "Comparison with Global Soil Radiocarbon Observations Indicates Needed Carbon Cycle Improvements in the E3SM Land Model."  Journal of Geophysical Research: Biogeosciences.  https://doi.org/10.1029/2018jg004795.