Urban environments cover a small fraction of the global surface (<3%); however, they noticeably affect local climate. Given most of the global population reside in urban areas (United Nations, 2019), improvements to weather forecast skill in these areas would have considerable societal benefits. The atmospheric impact of urbanization is multi-faceted and includes direct contributions to the urban heat island (UHI) effect from anthropogenic heating (Ao et al., 2018) and cooling (Takane et al., 2017). Buildings alter the surface morphology, whilst urban materials change the albedo, emissivity, and both thermal and hydrological properties of the surface. Other climatic impacts come from anthropogenic activities, including irrigation, drainage, snow-clearing and trace gas emissions. These components are known to impact, amongst other things, temperature, wind fields, surface heat and moisture fluxes, the boundary layer height and precipitation (Oke et al., 2017).Historically, urban areas were difficult to resolve in global numerical weather prediction (NWP) models, as they operated at a coarse horizontal resolution (>10 km). As model resolution increases (1-10 km) in systems such