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1 Introduction Terrestrial biogeochemical models usually contain several modules (e.g., photosynthesis, litter fall, carbon decomposition) by defining various state variables representing carbon and nitrogen pools to simulate the feedback of land ecosystem to global change over the past decades (Ahlström et al., 2012; Lehmann & Kleber, 2015; Wieder et al., 2018).
Uptake of anthropogenically emitted carbon (C) dioxide by terrestrial ecosystem is critical for determining future climate. However, Earth system models project large uncertainties in future C storage. To help identify sources of uncertainties in model predictions, this study develops a transient traceability framework to trace components of C storage dynamics. Transient C storage (X) can be decomposed into two components, C storage capacity (X ) and C storage potential (X ).
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