A cloudburst is the result of strong convective mechanisms. Due to its intensity, suddenness and brief duration, it is particularly difficult to adequately drain the resulting surface water, which accordingly may lead to severe flooding and consequently large economic losses. Such flash floods are not uncommon across the world and are devastating when occurring in a densely populated city such as Copenhagen, Denmark-even without additional complicating runoff effects from surrounding more elevated areas (Khajehei et al., 2020;Ricchi et al., 2021). Predicting the precise location, timing and intensity of weakly forced convective events (e.g., initiated by local surface conditions) is notoriously difficult, even for a state-of-the-art, convection permitting Numerical Weather Prediction (NWP) models due to a combination of (a) model resolution not fully resolving either the deep convection mechanism or local interactions related to orography or land/sea contrasts, (b) imprecise depiction of the initial conditions (IC) due to a lack of high-resolution observations (in particular of humidity) and (c) the chaotic behavior and associated sensitivity to IC of the atmosphere in general and convection in particular (Coppola