The fate and transport of pollutants in urban settings is dictated by numerous complex environmental processes. Urban microclimates, short pollutant travel times, and intricate flow routing around buildings make the identification of migration pathways and the quantification of contamination on surfaces and in storm water runoff challenging. Following a wide-area pathogenic biological release, such as of Bacillus anthracis (the causative agent of anthrax), consequence management activities including sampling, mitigation, decontamination, and waste management may last for many months (D'Amelio et al., 2015; Sinclair et al., 2008). Response strategies and resource management could benefit from a better understanding of the impact of rainfall on pollutant transport, but reference studies describing washoff do not exist for biothreat agents (Mikelonis et al., 2018). Washoff is the process of removing constituents from surfaces during a period of water runoff. It is a function of many factors including rainfall intensity and/or runoff volumes or rates (Rossman & Huber, 2016; Vaze & Chiew, 2003). For the case of particles, washoff has been mechanistically evaluated through the lens of sediment transport theory, where erosion is related to a critical shear stress that can initiate movement of the particle (Vanoni, 1975). However, several aspects of urban washoff are incongruent with the bulk of work developed for sediment transport. Urban overland flow is very shallow compared to flow in rivers, impervious materials represent a large fraction of surfaces, and rainfall energy in addition to the movement of overland flow can cause particle detachment and motion. Rainfall simulators have been used for decades as the primary means to study pollutant washoff both in the laboratory and in field settings (