Total streamflow across the Falls River was last observed at 657 cfs, and is expected to yield approximately 1,303 acre-ft of water today; about 53% of normal. River levels are low and may signify a drought. Average streamflow for this time of year is 1,239 cfs, with recent peaks last observed on 2011-06-09 when daily discharge volume was observed at 17,100 cfs.

Maximum discharge along the river is currently at the Falls River Nr Chester Id reporting a streamflow rate of 446 cfs. However, the streamgauge with the highest stage along the river is the Falls River Ab Yellowstone Canal Nr Squirrel Id with a gauge stage of 5.39 ft. This river is monitored from 4 different streamgauging stations along the Falls River, the highest being situated at an altitude of 5,777 ft, the Falls River Ab Yellowstone Canal Nr Squirrel Id.

The Falls River is a river that runs through the northeastern part of the United States, primarily in New Hampshire. It is approximately 32 miles long and flows into the Pemigewasset River. The hydrology of the river is characterized by a steep gradient and a high volume of water flow due to its location in the White Mountains. The river is fed by several smaller tributaries and contains several reservoirs and dams, including the Rocky Gorge Reservoir and the Lower Falls Dam. These reservoirs and dams are used for hydroelectric power generation, flood control, and recreation. The river is a popular destination for fishing, kayaking, and hiking. Additionally, the surrounding land is used for agriculture, primarily dairy farming. The history of the area dates back to the Native American tribes who lived along the river and later saw the arrival of colonial settlers in the 17th century.