Streamflow levels across
Virginia
are currently
46.0% of normal, with the
New River At Glen Lyn
reporting the highest discharge in the state with
2490cfs and gauge stage of 3.52 ft.
Meanwhile, the
Russell Fork At Haysi
is seeing a spike in streamflows today after experiencing a
168.46%
increase since yesterday, and currently running at
229cfs.
Maximum gauge stage in the state was last observed at the
Blackwater River Near Dendron, currently reporting a stage of
32.73ft.
The
Russell Fork At Bartlick
in the
Upper Levisa
watershed
is surging for this time of year at
1060cfs, about
45.34% of normal.
Virginia has a humid subtropical climate characterized by hot summers and mild winters. The state's major surface flows include the James, Potomac, and Rappahannock rivers, which are key sources of water for cities and industries. Virginia also has several major reservoirs and dams, including the Smith Mountain Lake and the John H. Kerr Reservoir. The state's hydrology is influenced by a variety of factors, including snowpack levels, precipitation patterns, and groundwater resources. In recent years, Virginia has experienced more frequent and severe flooding events due to increased precipitation and storm activity. Efforts are underway to improve water management and conservation practices throughout the state in response to these challenges.