Middle Neuse

Watershed Hydrology

The Middle Neuse Watershed (HUC 03020202) covers an area of approximately 2,880 square miles in central North Carolina. The region is characterized by rolling hills and numerous streams that feed into the Neuse River. The hydrology of the area is primarily controlled by the topography, which results in rapid runoff during heavy rainfall events. The watershed receives an average of 45 inches of snowfall annually, and the snowpack typically melts during the early spring months. The surface water in the area is of high quality and supports a diverse range of aquatic life. There are several reservoirs in the Middle Neuse Watershed, including Falls Lake and Jordan Lake, which provide drinking water and recreational opportunities for local communities. Interesting climatic facts include an increase in temperatures over the past century, with a significant number of record maximum temperatures occurring in recent decades. Additionally, the region has experienced an increase in extreme weather events such as hurricanes and heavy rainfall events. These trends may have implications for the hydrology and ecology of the Middle Neuse Watershed in the coming years.


Surface Flows

Middle Neuse Watershed

Snowpack Depths

Middle Neuse Watershed

Dams & Reservoirs

Middle Neuse Watershed

Groundwater Levels

Middle Neuse Watershed

Middle Neuse Rivers

Rivers of the Watershed