Streamflow levels across
North Carolina
are currently
39.0% of normal, with the
Pee Dee R Nr Rockingham
reporting the highest discharge in the state with
3990cfs and gauge stage of 2.99 ft.
Meanwhile, the
Valley River At Tomotla
is seeing a spike in streamflows today after experiencing a
61.18%
increase since yesterday, and currently running at
245cfs.
Maximum gauge stage in the state was last observed at the
Hyco Creek Near Leasburg, currently reporting a stage of
24.33ft.
The
Swift Creek At Hilliardston
in the
Upper Tar
watershed
is surging for this time of year at
858cfs, about
109.38% of normal.
North Carolina has a humid subtropical climate with distinct seasons that impact water flow conditions. The state is home to several major surface flows, including the Catawba River, Yadkin River, and Neuse River. These rivers are fed by numerous tributaries and are critical sources of drinking water and recreational activities. Major reservoirs such as Lake Norman and Falls Lake play important roles in managing water supply and mitigating floods. The state's hydrology is influenced by frequent rainfall, which can lead to flash floods and landslides. Snowpack in the Appalachian Mountains affects river flow in the spring and early summer. In recent years, North Carolina has experienced extreme weather events, including hurricanes, that pose significant challenges to managing water resources.