Streamflow levels across
Maine
are currently
76.0% of normal, with the
Penobscot River At West Enfield
reporting the highest discharge in the state with
26400cfs and gauge stage of 8.46 ft.
Meanwhile, the
Carrabassett River Near North Anson
is seeing a spike in streamflows today after experiencing a
153.04%
increase since yesterday, and currently running at
4580cfs.
Maximum gauge stage in the state was last observed at the
Mattawamkeag River Near Mattawamkeag, currently reporting a stage of
10.41ft.
The
Grand Lake Stream At Grand Lake Stream
in the
St. Croix
watershed
is surging for this time of year at
1240cfs, about
124.5% 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.