Churchill River above Wintego Rapids Water Level
Live river level, flow, historical records and forecast for Churchill River above Wintego Rapids in SK, Canada, built from official government gauge data.
- Location SK, Canada
- Watershed central churchill man highrock lake
- Primary gauge 06EA011 (Water Survey of Canada)
About Churchill River above Wintego Rapids
The Churchill River above Wintego Rapids is in the Central Churchill (Man.) - Highrock Lake watershed in Saskatchewan.
The watershed
This station watches the Churchill River with a drainage area upstream of 208500 km2 (80502 sq mi). That is the area feeding the gauge, not the whole watershed name on the map.
For people living along the river, the key point is that this site carries a long record: 40 years on record. That gives useful context when today’s level looks high or low on its own.
What the numbers say
The record high is 12.68 m (41.6 ft) in July 2020. The record low is 7.45 m (24.44 ft) in November 2025. Those two marks set the outer range this station has seen so far.
Seasonally, the highest typical month is July at 9.56 m (31.37 ft), while the lowest typical month is April at 8.97 m (29.42 ft). The typical annual swing is 59.6 cm (23.5 in). For docks, shore work, and intakes, that swing is the change to plan around through the year.
That seasonal pattern matters here because the prairie-style hydrograph often puts more water on the landscape in spring and then settles into a longer summer recession. On windy days, readings can also shift with setup on larger water bodies, so a single value is best treated as a snapshot, not the whole story.
Reading the hero number
The hero number on this page is most useful when you compare today’s reading with the median for the same calendar day across the station record. That tells you whether the river is running above or below its usual level for this date, which is more useful than raw elevation alone.
This station’s record comes from the Water Survey of Canada, and the comparison is stronger because it sits on more than 40 years of measurements.
How this page is built
Readings come from official government gauges and are rolled into daily records: the daily mean, high and low for every day on record. Each calendar day gets its own baseline from the full history, so the level you see is compared against what this specific date usually looks like rather than an annual average.
How Nibi Metrics works · Water stories
Nibi Metrics - live water levels, flow, and forecasts for lakes and rivers across Canada, the US and the UK
Real-time water levels, forecasts, and alerts for lakes and rivers across Canada, the US and the UK. Built on official government data.
Nibi Metrics tracks more than 13,000 gauged lakes and rivers across Canada, the United States and the United Kingdom, reading directly from official federal monitoring networks: the Water Survey of Canada, the United States Geological Survey, Quebec's provincial hydrometric network, and the Environment Agency for England. Every number on the platform is measured, not modelled - taken from a government gauge on the water itself and compared against that location's own historical record for this exact date.
What you can see for any monitored lake or river
The level right now, in feet or metres, updated as the source agency publishes new readings - for many stations that is every five to fifteen minutes. How today compares to typical: every location carries its own typical-for-this-date band built from its historical record, so a reading is never just a number - it is above, below, or near what this water usually does on this calendar day. Which way it is moving: a measured RISING, FALLING, or STEADY verdict computed from the gauge's own recent readings, with the rate of change - the difference between a flood ending and one beginning. What comes next: level forecasts up to 72 hours ahead, driven by the gauge's recent behaviour, upstream water, and quantitative precipitation forecasts, alongside live radar, lightning, and weather for the surrounding region.
Alerts that watch the water for you
Set a threshold on any location - a level, a distance above typical, or a rate of climb - and Nibi emails or notifies you the moment the gauge crosses it. Cottagers use it for spring freshet, anglers for river conditions, marinas and municipalities for operations. The scanning runs around the clock against the same measured data shown on every page.
Where Nibi comes from
Nibi means water in Anishinaabemowin. The platform began at a family cottage on Lake Muskoka, Ontario, where the spring melt floods the shoreline most years and the only forecast was standing on the dock, looking, and guessing. It grew into an independent, member-funded platform run by Muskoka Research Inc. - no investors, no data resale, and a privacy policy shorter than most cookie banners. The core data is free for everyone, forever; paid plans add automation like multi-location alerts, deep history, and reports.
Coverage
Nibi spans the continent: every Canadian province and territory with active federal gauges - from Vancouver Island rivers to the Muskoka lakes, prairie reservoirs, and Quebec's hydrometric network - and the United States from Maine to the Texas Hill Country, the Ohio Valley, and the Pacific Northwest. Coverage grows where the water news is: when a basin floods, its gauges join the platform with their full historical records attached. Many stations report every five to fifteen minutes; most report at least hourly; every page states exactly when its gauge last spoke.
Free forever, funded by members
The core promise is simple: the water data is free, for everyone, forever. Live levels, maps, radar, and recent history never sit behind a paywall. Paid plans fund the platform by adding automation - multi-location alerts, decades of history, longer forecasts, and PDF reports - so the people who need more carry the cost for everyone who just needs to check the lake before driving up. There are no investors and no advertising deals shaping what the data says.
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How every number is computed - About the platform
