Floods in the US exhibit strong spatiotemporal variability, mainly controlled by precipitation
types and catchment attributes. In a future warmer climate, it remains largely unclear how
such features change, relative to the current climate. Global Climate Models at coarse
resolution cannot resolve convective‐scale storms which is one of the major weather
systems causing devastating floods in the US. Alternatively, coupled, high‐resolution and
continental‐scale climate and flood simulations can advance our understanding. In this …