Streamflow levels across
Maine
are currently
31.0% of normal, with the
Penobscot River At West Enfield
reporting the highest discharge in the state with
3890cfs and gauge stage of 1.95 ft.
Meanwhile, the
St. John River At Ninemile Bridge
is seeing a spike in streamflows today after experiencing a
81.63%
increase since yesterday, and currently running at
1720cfs.
Maximum gauge stage in the state was last observed at the
Kennebec River At Bingham, currently reporting a stage of
7.54ft.
The
St. John River At Ninemile Bridge
in the
Upper St. John
watershed
is surging for this time of year at
1720cfs, about
-42.48% of normal.
Maine experiences varied flow conditions due to its unique hydrology and climate characteristics. Major surface flows include the Penobscot, Kennebec, Androscoggin, and Saco Rivers, which are regulated by large reservoirs and dams. The watershed area of each river is affected by snowpack, precipitation, and temperature, resulting in seasonal flow changes. Coastal rivers are influenced by tides and have a freshwater/saltwater interface. Maine's precipitation is relatively high, but its variability poses challenges in water management. Climate change may cause more extreme weather events, such as heavy rainfalls and droughts, affecting water availability and quality. As a result, monitoring and management of Maine's water resources are crucial for sustaining ecology, economy, and public well-being.
River Run | Status | Streamflow (CFS) | Air Temp (F) |
---|---|---|---|
Kennebec Gorge
Class III to IV+ |
44.67 |