There is considerable uncertainty right now about water levels and flows given the effects of ice on the Environment Canada gauges. This should resolve itself once we reach the open water season. The readings reported below are therefore tentative.
The level of Lake Manitoba rose 0.06 feet last week and is now over 813 feet again. The MIT forecast is for the lake to reach between 813.08 and 813.18 feet.
Flows on the Waterhen River are uncertain due to the effects of ice on the gauges. Once the ice clears, at the current level of Lake Winnipegosis, flow on the Waterhen will reach 7,500 cfs. MIT forecasts that the level of Lake Winnipegosis will peak between 833.01 and 833.40 feet. At these lake levels, flows on the Waterhen River will reach between 8,000 and 9,000 cfs.
Flow at Fairford is now 8,000 cfs. At the current level of Lake Manitoba, an unrestricted outflow at Fairford should be 10,600 cfs. However, because MIT has chosen to reduce outflows at Fairford over the winter, flows are 2,600 cfs below what they should be if lowering the level of Lake Manitoba was a priority.
Tomorrow will be the five-month anniversary of the reduction in flows at Fairford. When MIT announced that flows at Fairford were to be reduced last November, they stated that flows would be restricted for a 6-week period only.
With restricted outflows at Fairford, the level of Lake St. Martin is now falling quickly currently sitting at 801.21 feet, more than a quarter of a foot below last week’s level.
The pattern of flow on the Assiniboine is unclear and quite possibly ice affected. Flows on the Assiniboine at Holland are now 6,000 cfs. Flow on the Assiniboine at Headingly is currently under 3,000 cfs. What is curious is that on April 1st, the gauges indicated that flow at Headingly dropped sharply from about 6,000 cfs to under 3,000 cfs by the morning of April 2 and have remained near 3,000 cfs since then. If these values are accurate (and they may not be), it suggests that something happened and is continuing to happen between Holland and Headingly. The Portage Reservoir and Portage Diversion lie between Holland and Headingly.
Consistent with the drop in flow at Headingly, the level of the Portage Reservoir began to rise sharply on the 31st of March, rising a meter over the next day. Some of the flow reduction at Headingly appears to be explained by storing water in the Portage Reservoir. The level of the reservoir peaked on April 2 and has remained relatively stable since then. Obviously, what is not going down the Assiniboine or being stored in the reservoir is going down the Portage Diversion.
River update
Time: 9:00 AM April 5
Portage Diversion: open – gauge ice affected
Assiniboine at Holland: 6,001 cfs
Assiniboine at Headingly: 2,969 cfs
Waterhen: ice affected
Whitemud: 847 cfs
Fairford: 8,013 cfs
Lake update
Time: 9:00 AM April 5
Steep Rock: 813.06 ft
Westbourne: 812.96 ft
Mean level: 813.01 ft
Lake St. Martin: 801.21 ft