MAINE FLOW REPORT

Last Updated: January 11, 2026

The state of Maine's river systems are currently experiencing varying degrees of streamflow changes, with many rivers reporting below-normal flows, which are significant for water enthusiasts, anglers, and environmental managers alike. Notably, rivers such as the Penobscot River at West Enfield are reporting a higher than normal streamflow at 26,800 cubic feet per second (cfs), which is 69.26% above the norm, potentially indicating flooding or high water conditions that could impact local communities and ecosystems. Conversely, the majority of the rivers, including the Kennebec, Androscoggin, and St. John Rivers, are experiencing lower than usual streamflows, with reductions of up to -86.71% from the normal at the Carrabassett River Near North Anson. This could indicate flow droughts in various watersheds, which might affect recreational water activities and local water resources.

Specifically, the St. John River at Dickey, a prominent river in the region, shows a streamflow of 1600 cfs, a significant decrease of -61.92% from what's typical for the area, with a corresponding gage height of 6.04 feet. For whitewater enthusiasts, the reduced flows may impact the rafting conditions on popular trails. The recent dramatic increase in streamflow on the Meduxnekeag River Above South Branch near Houlton, with a jump of 573.89 cfs in the last 24 hours, serves as a stark contrast to the generally low flows and highlights the variability that can occur in river systems. Meanwhile, the Penobscot, a critical river for both recreation and local economies, shows a substantial increase at West Enfield, warranting attention for potential flooding impacts near cities like Enfield and downstream communities. These dynamic conditions across Maine's river systems underscore the importance of monitoring streamflow data for safety, water resource management, and the preservation of the state's natural aquatic ecosystems.