Total streamflow across the Missisquoi River was last observed at 15,870 cfs, and is expected to yield approximately 31,478 acre-ft of water today; about 212% of normal. River levels are high. Average streamflow for this time of year is 7,471 cfs, with recent peaks last observed on 2014-04-16 when daily discharge volume was observed at 48,450 cfs.

Maximum discharge along the river is currently at the Missisquoi River At Swanton reporting a streamflow rate of 9,780 cfs. However, the streamgauge with the highest stage along the river is the Missisquoi River Near East Berkshire with a gauge stage of 7.37 ft. This river is monitored from 3 different streamgauging stations along the Missisquoi River, the highest being situated at an altitude of 598 ft, the Missisquoi River Near North Troy.

The Missisquoi River is a 80-mile-long tributary of Lake Champlain that flows through Vermont and Quebec. It was a crucial trade and transportation route for Native American tribes and early European settlers. The river has a hydrological history of flooding and ice jams, which led to the construction of several reservoirs and dams, including the Gorge Dam and Enosburg Falls Dam. These dams have helped to regulate water flow, prevent flooding, and generate hydroelectric power. The river is used for recreational activities such as fishing, kayaking, and swimming. It also supports agriculture, with farms located along its banks using its water for irrigation. The Missisquoi River is an important part of Vermont's history and provides valuable resources to the surrounding communities.