05/05/2026 | Press release | Distributed by Public on 05/05/2026 15:40
The Board expects the total St. Marys River flow in May to be 2,140 m3/s (75,600 ft3/s) as prescribed by Regulation Plan 2012.
The gate setting of the Compensating Works at the head of the St. Marys Rapids will be increased from the current setting equivalent to approximately one-half gate open to a setting equivalent to approximately four gates open, to meet the Plan 2012-prescirbed flow in May in consideration of capacity restrictions at the hydropower plants. On Thursday, May 7, Gates #7 through #12 will be raised to a setting of 1.22 meters (4 feet) open. Gate #1 will remain at its typical setting which supplies a flow of about 15 m3/s (500 ft3/s) to the channel north of the Fishery Remedial Dike. The St. Marys Rapids flow will increase from approximately 87 m3/s to approximately 534 m3/s after gate adjustments.
Water level changes over the month of April
There was a record rise in Lake Michigan-Huron water levels during April - this is based on historical records back to 1918 (109 years). Snowmelt runoff, combined with significant rainfall passing directly over the lake, were the main drivers for the record increase in water level.
Water levels as of the beginning of May
While the water level increases in April 2026 were significant, both lakes Superior and Michigan-Huron started the month below average. As a result, as of the beginning of May, water levels for both lakes are within 4 cm of their long-term averages.
Overall, considering the near average water level conditions on both lakes, outflows from Lake Superior into Lake Michigan-Huron will also be near average for the month of May.
Forecast outlook in May
The International Lake Superior Board of Control is responsible for managing the control works on the St. Marys River and regulating the outflow from Lake Superior into Lake Michigan-Huron. Under any outflow regulation plan, the ability to regulate the flow through the St. Marys River does not mean that full control of the water levels of Lake Superior and Lake Michigan-Huron is possible. This is because the major factors affecting water supply to the Great Lakes (i.e. precipitation, evaporation, and runoff) cannot be controlled and are difficult to accurately predict. Outflow management cannot eliminate the risk of extreme water levels occurring during periods of severe weather and water supply conditions. Actual flows will vary hour-to-hour and day-to-day depending on hydrologic conditions and variations in flow at the hydropower facilities. Additional information can be found on the Board's homepage: https://ijc.org/en/lsbc.