Last Updated: December 23, 2025
Vermont's rivers exhibit a range of streamflow conditions, with most basins reporting below-normal flows, showing a widespread pattern of reduced water activity that could affect recreational and environmental interests across the state. Notably, the Connecticut River at Wells River, a major watercourse with significance for both ecology and recreation, is flowing at 2,840 cubic feet per second (cfs), which has decreased by 29 cfs in the last 24 hours and is at only 45.49% of its normal flow. This trend is representative of other key rivers such as the Passumpsic, Wells, Ottauquechee, and White Rivers, all of which are experiencing reduced streamflow, with current measurements ranging from 74.61% below normal on the Passumpsic to 58.66% below on the Wells River. Consequently, whitewater enthusiasts should exercise caution given the potential for lower river levels and exposed hazards, while municipalities and environmental managers may need to consider the implications for water supply and aquatic habitat health.
In contrast, the Mad River near Moretown displayed a 54.65 cfs increase in streamflow, which could indicate localized rising water levels, albeit still at 28.19% below the normal flow rate. This unusual spike may be of interest to paddlers looking for rapids but also flags a potential for flash flooding in surrounding areas. The Black River at North Springfield and the Poultney River below Fair Haven have seen increases of 26.81 cfs and 21.85 cfs, respectively, suggesting localized influxes in water volume. Such changes could affect nearby cities like Springfield and communities along the Poultney River, signaling a need for vigilance. The Otter Creek at Middlebury, another significant waterway for both recreation and local ecosystems, is near normal flow levels at 13.37% below average, possibly maintaining better conditions for river activities. Overall, Vermont's rivers demonstrate a patchwork of below-normal streamflows with isolated increases, underscoring the importance of close monitoring for water-related recreation and management throughout the state.
Vermont's flow conditions are influenced by its hydrology and climate characteristics. The major surface flows in the state include the Connecticut River, Lake Champlain, and the Winooski River. These surface flows are often impacted by snowpack and rainfall in the watersheds that feed them. Vermont's reservoirs and dams, such as the Waterbury Reservoir and the Northfield Falls Dam, play an important role in regulating flow and providing hydroelectric power. The state also experiences occasional flooding, particularly in the spring when snowmelt combines with heavy rainfall. To manage these risks, Vermont has implemented a statewide flood hazard mitigation program. Overall, Vermont's flow conditions are complex and dynamic, reflecting the state's unique topography, climate, and water resources.
Residents in Bennington and Western Windham Counties in Vermont should prepare for a wintry mix of weather conditions, including snow accumulations of 2 to 5 inches, with up to 7 to 8 inches possible along the southern Greens. Additionally, patchy freezing drizzle may create a light glaze of ice. The Winter Weather Advisory is in effect from 7 AM Tuesday until 7 AM Wednesday. Travel could become difficult, particularly during the Tuesday morning and evening commutes, with potential reduced visibility and slippery roads due to falling snow and gusty northwest winds. People in the affected areas should exercise caution and consider adjusting travel plans.