Populated urban areas tend to be located in sedimentary basins with broad flat land and favorable positions near water bodies (Wirth et al., 2019). However, shallow soft sediments with low shear velocity can trap seismic energy and amplify earthquake shaking (Aki, 1993;Singh et al., 1988). Characterizing near-surface structure and quantifying ground motion is critical to mapping the seismic risk of urban regions. Estimating seismic hazard is usually accomplished with empirically derived ground-motion models (GMMs) with site characteristics, usually Vs30 (the time-averaged shear velocity in the upper 30 meters), which can be empirically inferred from local tomography models, geologic units, and topography gradients, but is often sparse and uneven spatially (Allen