Abstract Atmospheric deposition of dissolved inorganic phosphorus (DIP) is crucial to nutrient cycling but remains poorly constrained in chemical transport models (CTMs). Large uncertainties in phosphorus emissions and aerosol dissolution processes challenge the reliable estimates of DIP fluxes. Here, we developed a two‐stage random forest residual learning framework integrating observational DIP data sets with CTM simulation outputs. Compared to the original CTM results, our machine learning model substantially narrows the gap of DIP deposition fluxes across the globe between the observations and model estimates, with improved Pearson correlation from 0.10 to 0.85. The optimized global DIP deposition is estimated of 2.02 Tg DIP yr −1 , with a 95% confidence interval of 1.98–2.59 Tg DIP yr −1 . Our estimate is 60%–460% higher than the CTM‐based estimates from previous studies. In particular, 1.35 Tg DIP yr −1 (67%) is deposited over land and 0.67 Tg DIP yr −1 (33%) over ocean. The sourc
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