Kitimat River below Hirsch Creek Water Level

Live river level, flow, historical records and forecast for Kitimat River below Hirsch Creek in BC, Canada, built from official government gauge data.

About Kitimat River below Hirsch Creek

Kitimat River below Hirsch Creek sits in the Hecate Strait - Kitimat watershed in British Columbia.

What the record shows

The record on this station spans more than 60 years. The highest level in that span was 4.8 m (15.75 ft) in October 2017. The lowest was -0.07 m (-0.23 ft) in January 2011.

The seasonal pattern is clear. Typical levels peak in May at 1.61 m (5.28 ft), then ease to a typical low in March at 0.73 m (2.38 ft). That is a typical annual swing of 88.4 cm (34.8 in). For anyone with a dock, intake, or bank access point, that is the range to plan around each year.

No fastest 24-hour rise is listed here, so there is no movement figure to use for short-notice change on this page.

The watershed

The drainage area above this gauge is 1,999 km2 (772 sq mi). That is the area contributing flow to this station, not the full watershed on a map.

For a river in mountain country, the seasonal shape matters. Spring levels rise toward May, then the river falls back through the rest of the warm season. That pattern is what matters for launching, shoreline access, and any fixed intake sitting near the waterline.

The record high in October 2017 and the record low in January 2011 show that this site can sit near the edges of its range in different parts of the year. That is worth keeping in mind if you use the river every day or only check it when conditions change.

Reading the hero number

The number shown at the top of the page is today’s reading compared with the median for this calendar day across the station record. That is more useful than raw elevation because it tells you whether the river is running high or low for this date, not just how far it sits above sea level.

With more than 60 years on record, the calendar-day median gives a steadier reference for local use: a quick read on whether this water is acting like it usually does for the season.

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

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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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