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Nibi Metrics

Real-time water levels, forecasts, and alerts for lakes and rivers across Canada and the US. Built on official government data.

Nibi Metrics turns raw gauge readings from official hydrometric networks into something a person standing on a dock can actually use: is the water high or low for today, which way is it moving, and how unusual is this? This page explains where every number on the platform comes from and what we do to it along the way.

Water Stories

The flood of record that was overtaken

For five years, spring 2019 was the mark every Lake Muskoka decision answered to. In April 2026 the lake went two centimeters higher - and the official books have not caught up yet.

Why the Assiniboine floods every spring

Inside the freshet cycle that puts Manitoba shorelines at risk each year - and why 2026 broke the script.

How snowpack becomes summer water

The science of snow water equivalent and why it drives the season ahead.

Reading a staff gauge like a hydrologist

What the numbers on the measuring stick actually tell you.

Flash Flood Alley: how Texas rivers rise in hours

Why Central and South Texas rivers go from gravel beds to fifty-year records in an afternoon - including July 2026 on the Nueces.

What a "100-year flood" actually means

One percent, every year, forever - unwrapping hydrology's most misunderstood phrase, and how it differs from our own percentiles.

Athabasca River at Hinton Water Level

Live river level, flow, historical records and forecast for Athabasca River at Hinton in Canada, AB, Canada, built from official government gauge data.

About Athabasca River at Hinton

Athabasca River - A vital waterway in Alberta's foothills.

The Athabasca River at Hinton flows through a significant stretch of the Upper Athabasca - Oldman watershed, characterized by its expansive drainage area of roughly 9,820 square kilometres. This river is an essential natural resource, drawing on the hydrology of the foothills and prairie regions of Alberta.

The watershed context

Hinton, nestled in close proximity to the Canadian Rocky Mountains, is influenced by a distinct seasonal rhythm defined by mountain snowmelt that contributes to late-spring water levels. As the snowpack melts, usually peaking towards the end of spring, the flow rates in the Athabasca River can rise significantly. During summer, convective storms may further enhance river flows, resulting in sharp increases following heavy rainfall.

The Athabasca River runs approximately through a region that combines both foothills and adjacent prairie landscapes, illustrating the diversity of Alberta’s ecology and hydrology. This river serves not only as a water source but also as an ecological corridor, supporting various wildlife and plant species along its banks.

Why the data matters here

Monitoring the Athabasca River's flow is vital for several reasons. Water levels affect local ecosystems, recreational activities, and flood management efforts. The station at Hinton records discharge measurements, providing important data about current conditions.

Today, the river's reading will be compared against historical data: this gauge's measurement is contrasted with the median for this calendar day over the past 49 years. Such comparisons are crucial; they give a better understanding of whether today's water level is typical or notable compared to its historical patterns. The data is managed by Water Survey of Canada, ensuring accurate and reliable records for all users who depend on the Athabasca River's health and status.

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