Understanding flow and transport processes at large scales (e.g., field) has always been challenging due to spatial and temporal variations and complexities. Accordingly, upscaling approaches have been widely applied to determine the value of a property at a larger scale (e.g., field) from available characteristics at a smaller scale (e.g., core). Due to its broad practical applications, upscaling has been an active subject of research in various research areas, such as hydrology, civil, chemical and petroleum engineering, and soil physics.One of the most important hydraulic and petrophysical properties of porous media is permeability, the capability of a soil or rock to allow the passage of fluid through it. Therefore, over the past decades, numerous studies focused on its modeling and estimation across scales. For instance, at the core scale, permeability can be estimated either from pore-scale properties, such as pore-throat radius distribution (