DELAWARE FLOW REPORT
Last Updated: January 2, 2026
Brandywine Creek, a significant waterway in Wilmington, Delaware, currently exhibits a streamflow of 160 cubic feet per second (cfs), which is significantly below the seasonal norm by 76.24%. This considerable deviation suggests that the creek is experiencing a flow drought, which may affect river activities such as fishing and boating. The current gage height is recorded at 8.47 feet, and over the past 24 hours, there has been no change in streamflow. This information is pertinent for water enthusiasts who frequent the Brandywine Creek, as it is a notable river for its recreational value and ecological significance in the state.
The lack of a significant increase in streamflow suggests that there is no immediate threat of flooding in the Brandywine Creek area. However, the abnormally low streamflow could have implications for the ecosystems within the creek and downstream areas, possibly impacting wildlife and plant life that depend on the waterway. Seasonal trends such as these might also influence water quality, availability of water resources, and the enjoyment of whitewater trails along the creek. Residents and visitors in Wilmington and surrounding communities should be aware of these conditions, as low water levels can alter the character and accessibility of the creek for recreational use. It's essential for river and water enthusiasts to monitor these trends and plan their activities accordingly, taking into account the current state of the Brandywine Creek and being cognizant of potential changes in the near future.
Delaware has a humid subtropical climate with moderate rainfall throughout the year. Major surface flows in Delaware include the Delaware River, the Brandywine Creek, and the Christina River. The Chesapeake Bay also borders the state. Major reservoirs include the Kent County Water Supply and the Betts Pond. The state is susceptible to coastal flooding and inland flooding due to heavy rainfall. Watershed data indicates that most of the state is within the Delaware River Basin, although small portions are within the Chesapeake Bay and the Atlantic Ocean Basins. Snowpack is typically low in Delaware due to the warm winter temperatures. Overall, the hydrology of Delaware is influenced by its coastal location, moderate rainfall, and dominant surface flows.