Spatiotemporal distribution of global rainfall has changed significantly in response to anthropogenic modifications of the natural environment (Marvel & Bonfils, 2013). Record-breaking rainfall events have been increasingly observed during the past decades (Lehmann et al., 2015), with even more frequent intense rainfall expected under a warming globe in the future (Min et al., 2011;Moustakis et al., 2021). Cities are particularly vulnerable to heavy rainfall because the expansion of impervious materials increases runoff volumes and subsequently elevates flood risk within urban areas (L. Yang, Smith, & Niyogi, 2019). Additionally, by modifying land surface energy and moisture balances, cities themselves have notable impacts on regional rainfall through land-atmosphere interactions. A meta-analysis concluded that urbanization enhances mean rainfall by 18% downwind of the city and by 16% over the city (Liu & Niyogi, 2019). The urban-induced rainfall anomalies could substantially increase urban flood risks (Huong & Pathirana, 2013;L. Yang, Smith, & Niyogi, 2019). As global urbanization trend will continue in the foreseeable future, it is imperative to understand urban rainfall modification so as to develop effective adaptation strategies for urban flood risks (Hemmati et al., 2020).