Total streamflow across the Williams River was last observed at 480 cfs, and is expected to yield approximately 952 acre-ft of water today; about 97% of normal. Average streamflow for this time of year is 496 cfs, with recent peaks last observed on 2014-05-16 when daily discharge volume was observed at 7,590 cfs.

Maximum discharge along the river is currently at the Williams River At Dyer reporting a streamflow rate of 480 cfs. This is also the highest stage along the Williams River, with a gauge stage of 2.91 ft at this location. This river is monitored from 2 different streamgauging stations along the Williams River, the highest being situated at an altitude of 2,198 ft, the Williams River At Dyer.

The Williams River is a 33-mile-long river located in the eastern part of Vermont. The river flows through the towns of Rockingham, Chester, and Springfield, and eventually empties into the Connecticut River. The Williams River is known for its historic significance, as it played an important role in the development of the region's industry and transportation. The river is dammed at several points, including the Lower Williams Dam, which was built in 1909 to generate hydropower. The Williams River is also home to the Ball Mountain Dam, which creates the Ball Mountain Reservoir - a popular recreational spot for swimming, boating, and fishing. The river is used for agricultural purposes, including irrigation and livestock watering. Overall, the Williams River is an important resource for both the local economy and recreational opportunities.