“…These processes lie in the “gray zone,” with scales O (1–100 km) which are under‐resolved in typical climate models but are largely resolved in computationally intensive sub‐kilometer scale models (e.g., atmospheric subgrid momentum fluxes: Yuval & O’Gorman, 2020; Yuval et al., 2021; Wang et al., 2022; ocean momentum forcing: Guillaumin & Zanna, 2021; Perezhogin et al., 2023; convection: Brenowitz & Bretherton, 2019; Gentine et al., 2018; clouds: Rasp et al., 2018; gravity waves: Sun et al., 2023) or large eddy simulations (e.g., eddy‐diffusivity momentum flux: Lopez‐Gomez et al., 2022; Shen et al., 2022). However, other coupled processes such as atmospheric chemistry, sea ice cover, and vegetation dynamics are not modeled explicitly at any resolution and may make use of observational data sets (e.g., ozone: Nowack et al., 2018; sea‐ice: Andersson et al., 2021; vegetation: Chen et al., 2021). Alternatively, some studies simply use ML to emulate existing parameterizations at a lower computational cost (e.g., radiation: Chevallier et al., 1998; Krasnopolsky et al., 2005; aerosol microphysics: Harder et al., 2022; cloud microphysics: Andre Perkins et al., 2023).…”