Total streamflow across the
Aroostook River
was last observed at
562
cfs, and is expected to yield approximately
1,115
acre-ft of water today; about 14%
of normal.
River levels are low and may signify a drought.
Average streamflow for this time of year is
4,123 cfs,
with recent peaks last observed
on
2018-04-28 when daily discharge volume was observed at
63,100 cfs.
Maximum discharge along the river is currently at the
Aroostook River At Washburn
reporting a streamflow rate of 371 cfs.
However, the streamgauge with the highest stage along the river is the
Aroostook River Near Masardis
with a gauge stage of 2.77 ft.
This river is monitored from 2 different streamgauging stations along the Aroostook River, the highest being situated at an altitude of 542 ft, the
Aroostook River Near Masardis.
The Aroostook River, located in Maine, is approximately 110 miles long and flows into the St. John River. The river has a rich history, being an important transportation route for Native Americans and later for lumber and agriculture industries. The hydrology of the river is influenced by the surrounding forests and wetlands, which play a critical role in regulating water flow and maintaining water quality. There are several dams and reservoirs along the river, including the Masardis Dam, which provides hydroelectric power and flood control. The river is also used for recreational activities such as fishing, kayaking, and camping. Additionally, the fertile soils along the river support agricultural production including potato farming. The Aroostook River is an important resource for both industry and recreation in the state of Maine.