Figure 2. Modeled tidal inundation of two stormwater networks in downtown Beaufort during the study period. The average percent fill of stormwater catchments (attached to subterranean pipes) is shown for lower low tide (2a,c) and higher high tide (2b,d) for the baseline data collected from June 6 to August 2, 2022 (2a,b), and for the perigean tide data collected on June 12-17 and July 11-16, 2022 (2c,d).
Our pipe network model only accounts for variation in tidal elevation, as measured by the nearby NOAA tide gauge, and does not consider water level contributions from rainfall runoff, groundwater infiltration into the stormwater network, or pipe hydraulics. Bathtub models, like the pipe network model used here, typically overestimate flooding compared to models that account for pipe hydraulics (e.g., Castrucci & Tahvildari, 2018; Gallien et al., 2014). However, outside of rain events, Gold et al. (2023) showed that water levels in the Queen Street network track well with water levels measured at the NOAA tides gauge during baseline conditions, indicating that contributions from groundwater infiltration into the stormwater network are likely small for the pipe network. During rainfall events, the pipe network model is an underestimate of actual inundation.
While the network inundation model does not consider non-tidal forcing and pipe hydraulics, it can be used to estimate where inundation was relatively high and low across the network due to tidal forcing alone. In particular, the network inundation estimates highlight that total network inundation and roadway flooding were most likely to occur in and along the Queen Street network. The pipe network model also reveals that the Orange Street network experienced daily and major inundation, but to a lesser extent than the Queen Street network. Due to the inlet and outfall elevations not being surveyed, we are unable to assess the frequency at which the museum network was inundated.
3.2 Daily waterway ENT concentrations differed between sampling locations
ENT was detected in 73% of daily, or baseline, samples (n = 241/330) with concentrations ranging from 10 to 5,298 MPN 100 mL-1 (Fig 3). ENT measurements exceeded the single sample maximum threshold concentration for safe public use of recreational waters (104 MPN 100 mL-1) in 16% of the daily samples, indicating recurring but infrequent levels of unsafe fecal contamination in the waterway during the two month summer sampling period. Similar daily ENT concentrations in the waterway were observed between non-perigean and perigean tide periods. Hence, while perigean tide events lead to increased stormwater network inundation (Fig 2d), they did not necessarily result in increased ENT loading within the waterway.