Estimating streamflow and base flow within the nontidal Chesapeake Bay riverine system

Patrick C. Buffington; Paul D. Capel

doi:10.3133/sir20205055

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Estimating streamflow and base flow within the nontidal Chesapeake Bay riverine system

Patrick C. Buffington·Paul D. Capel

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Abstract

Daily mean streamflow was estimated for all the nontidal parts of the Chesapeake Bay riverine system with the Unit Flows in Networks of Channels computer application using measured streamflow at the most downstream gage of selected rivers. The streamflows estimated by the Unit Flows in Networks of Channels computer application were aggregated at the 12-digit Hydrologic Unit Code level, after which base flow was estimated by two hydrograph-separation methods. Based on six sites selected for comparison, modeled streamflows are typically within an order of magnitude of measured streamflows, and monthly mean streamflows are in better agreement than daily streamflows. For the six selected sites, the base-flow values calculated by the two hydrograph-separation methods were compared. The monthly base-flow values also were in better agreement than the daily base-flow values. The modeled data were animated to better visualize spatial and temporal variability of streamflow and base-flow index.

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Source-reported bounding extent: 36.48314061639213° to 42.98053954751642° latitude; -80.771484375° to -74.278564453125° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeX RIS

Patrick C. Buffington, Paul D. Capel. 2020-07-30. Estimating streamflow and base flow within the nontidal Chesapeake Bay riverine system. https://doi.org/10.3133/sir20205055

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