Second, we employed simple dynamical systems analysis to derive the relationship between subsurface storage and streamflow for three Baltimore, Maryland watersheds (3.8–14 km 2 in area) along an urban-to-rural gradient. First, we used a three-dimensional model of integrated subsurface and surface flow and solute transport to simulate an idealized hillslope to perform model-based chemical hydrograph separation of stormflow. We used multiple lines of inquiry to explore the relationship between pre-event water proportion, subsurface storage, and streamflow under storm conditions. ![]() Subsurface storage as a regulator of streamflow was investigated as an explanation for the large proportion of pre-event water observed in urban streams during storm events.
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