Streamflow levels across
Maine
are currently
79.0% of normal, with the
Penobscot River At West Enfield
reporting the highest discharge in the state with
17400cfs and gauge stage of 6.44 ft.
Meanwhile, the
North Branch Penobscot River Nr Pittston Farm
is seeing a spike in streamflows today after experiencing a
149.51%
increase since yesterday, and currently running at
2570cfs.
Maximum gauge stage in the state was last observed at the
Narraguagus River At Cherryfield, currently reporting a stage of
9.51ft.
The
North Branch Penobscot River Nr Pittston Farm
in the
West Branch Penobscot
watershed
is surging for this time of year at
2570cfs, about
197.11% 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.