Seminar: Qi Yang

Data-driven upscaling of biogenic fluxes from eddy covariance (EC) sites to the global scale is a powerful complementary approach to process-based models for the derivation of global flux estimates. Nevertheless, significant uncertainties arise due to specific methodological choices such as data availability, data source differences, machine learning model differences, and feature selection. In this study, we introduce a comprehensive framework for quantifying the uncertainties associated with carbon flux upscaling across potential sources. The framework involves three key steps: (1) proposing potential ensemble, (2) screening, and (3) uncertainty attribution. First, we evaluate potential ensemble members by training machine learning models with varying configurations, such as various feature combinations and subsets of EC sites. The experiments are supported by the recently developed data-driven modeling framework FLUXCOM-X, which enables a wide range of experiments with diverse methodological choices. We crafted a feature set that includes 316 features to capture both current and historical state information. To capture the site representativeness uncertainty, we sample subsets from global EC sites based on geolocation and feature space. Additionally, we will also investigate different machine learning models and the variation of hyperparameters to generate the ensemble. Second, ensemble members that have a low contribution to the ensemble variance will be eliminated while we retain the most representative ones. We employ a feature selection algorithm, HybridGA, to screen important subfeature sets from near-infinite combinations. Moreover, we screen other ensemble members by assessing the distribution and spread of members. Finally, we will attribute uncertainties to various categories from the perspectives of machine learning and process-based modeling, and potential strategies to reduce these uncertainties are discussed. The framework is initially used to evaluate spatiotemporal NEE uncertain patterns in Europe, and will subsequently expand globally. Additionally, the estimated biogenic carbon flux uncertainty will be assessed with independent products. This work not only advances our understanding of the sources and patterns of upscaled flux uncertainties but also will facilitate the atmospheric inversions in ITMS module M.