WHAT'S HAPPENING NOW
—— ft above typical
Finding the top signal on the water…
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Live river level, flow, historical records and forecast for Inkaneep Creek near the Mouth in Canada, BC, Canada, built from official government gauge data.
Inkaneep Creek is in the Okanagan watershed in British Columbia.
This station drains 184 km2 (71 sq mi) upstream of the gauge, so the numbers here describe what is happening above this point on Inkaneep Creek, not the whole watershed.
For someone watching a ditch, intake, or bank near the mouth, the main pattern is seasonal. The highest month is May, with a typical level of 1.74 m (5.71 ft), and the lowest month is August, with a typical level of 1.31 m (4.3 ft). That typical annual swing is 43.1 cm (17 in), which is the range a dock or small intake has to live with most years.
The record high is 2.72 m (8.91 ft) in May 2011. The record low is 1.09 m (3.58 ft) in January 2024. The fastest 24-hour rise on record is 31.9 cm (12.6 in) in May 2017, and the fastest 24-hour drop is 37.3 cm (14.7 in) in May 2023.
This is a mountain creek, so the seasonal shape fits the regional note: freshet builds in spring and often peaks from May through July. Here, the data show the high month in May and the low month in August, with a fairly tight typical swing of 43.1 cm (17 in). That means the channel can change enough over the season to matter for shallow crossings, pumps, and bank access.
The one-day rise of 31.9 cm (12.6 in) in May 2017 is the clearest warning number in the record. It tells you how quickly the creek can come up when conditions change. The one-day drop of 37.3 cm (14.7 in) in May 2023 shows the other side of that same volatility.
With 19 years on record, these are useful local benchmarks, not guesses.
The hero number on this page is today’s reading compared with the median for this calendar day across the station record. That is better than raw elevation because a level only matters when you know what is normal for this date.
The station is operated in the Water Survey of Canada network. With 19 years on record, the median gives a fair read on whether Inkaneep Creek is sitting low, near typical, or high for today.
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.
Real-time water levels, forecasts, and alerts for lakes and rivers in a growing number of countries. Built on official government data.
Nibi Metrics tracks more than 17,900 gauged lakes and rivers in a growing number of countries, reading directly from official federal monitoring networks: the Water Survey of Canada, the United States Geological Survey, Quebec's provincial hydrometric network, the Environment Agency for England, the Scottish Environment Protection Agency, Natural Resources Wales, the Office of Public Works in Ireland (waterlevel.ie), the Norwegian Water Resources and Energy Directorate (NVE), the State of Queensland's water monitoring network, and on the Great Lakes the Canadian Hydrographic Service and NOAA. 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.
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.
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.
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.
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.
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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