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Boreal forests play a critical role in the global carbon cycle as they are one of the largest terrestrial carbon sinks globally. In this study, we employ explainable machine learning (ML) techniques to investigate the influence of environmental and vegetation variables on net ecosystem exchange (NEE), focusing specifically on the effects of diffuse radiation. We utilize a sub-hourly resolution data set including satellite and in-situ observations from three boreal or hemiboreal forest research stations across the latitudes 58–68° N to capture latitudinal variability in forest carbon uptake. Using SHAP (Shapley Additive Explanations) values, we identify key drivers influencing NEE and quantify their importance across various ML model architectures. Photosynthetically active radiation (PAR), diffuse radiation, normalized difference vegetation index, and soil temperature were identified as the variables having the largest explanatory power for NEE across the ML models. ML models using only these variables result in R 2 ≈ 0.8 R²≈ 0.8 upper R 2 almost equals 0.8 and RMSE ≈ 2.3 ≈ 2.3 almost equals 2.3 μ mol m − 2 s − 1 μ mol\;m⁻²0.1em s⁻¹ mu molm minus 2 s minus 1 . Further analysis of SHAP values indicates that higher diffuse radiation (DiffPAR) is associated with more negative NEE (stronger carbon sink). SHAP analysis highlights this effect much more clearly than raw DiffPAR measurements, because it accounts for interactions with other environmental factors. This suggests that the diffuse radiation effect emerges from interactions between DiffPAR and co-varying environmental factors (such as cloudiness and total PAR). Cases identified by SHAP ( DiffPAR SHAP < − 2 DiffPAR\ SHAP<-2 DiffPAR SHAP less than minus 2 ) have a median NEE 1.55 μ mol , m − 2 , s − 1 1.55μ mol,m⁻²,s⁻¹ 1.55 mu mol comma m minus 2 comma s minus 1 more negative than cases with raw DiffPAR ≥ 400 DiffPAR≥ 400
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Laanti et al. (2026) studied this question.
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