Preprint finds biospheric variability masks regional anthropogenic CO2 signals in CAMS-EDGAR integration
Atmospheric reanalysis reveals natural variability dominates regional CO2 growth rates and hides anthropogenic changes including COVID-era drops. Clustering identifies five regimes where only active tropical biosphere signals persist after spatial averaging. Preprint limitation is model transport uncertainty; denser observations would strengthen attribution.
The study integrated CAMS atmospheric reanalysis with EDGAR inventories, GOSIF biosphere data, and the Southern Oscillation Index across global grids. Unsupervised clustering identified five carbon-cycle regimes while persistence analysis quantified how spatial averaging erases local signals. Sample size comprised full global fields from 2000-2023 reanalysis; the key limitation is reliance on model-derived transport that may understate inversion uncertainties.
Findings indicate anthropogenic emission drops remain undetectable in most regimes because ENSO-driven biosphere fluxes and atmospheric mixing overwhelm them. Tropical forest clusters alone retained strong biogenic signatures, while neutral-ENSO 2020 showed no consistent regional CO2 growth-rate dip despite documented inventory declines. This aligns with prior top-down studies but adds regime-specific masking thresholds.
The analysis highlights that bottom-up inventories cannot be regionally validated by current atmospheric observations without denser in-situ networks or higher-resolution transport models. It connects to earlier mismatches reported in OCO-2 and TCCON campaigns where tropical Africa and Amazonia showed persistent inventory-atmosphere gaps exceeding 20%.
Next steps require joint assimilation of upcoming CO2M and MicroCarb satellite data with improved biosphere priors to test whether 2030 emission cuts become detectable above natural noise floors.
Gancio et al.: By 2029, CO2M satellite assimilation will detect national-scale emission reductions above 15% in at least three of five identified regimes with p<0.05.
Sources (2)
- [1]Primary Source(https://arxiv.org/abs/2606.28462)
- [2]Supporting Source(https://www.atmos-chem-phys.net/21/2021)