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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.

Similkameen River at Princeton Water Level

Live river level, flow, historical records and forecast for Similkameen River at Princeton in Canada, BC, Canada, built from official government gauge data.

About Similkameen River at Princeton

Similkameen River - An essential waterway of the Similkameen Valley.

The Similkameen River at Princeton serves as a vital water resource flowing through British Columbia's scenic landscape. Draining approximately 1,810 square kilometres, the river plays a crucial role in the region’s ecology and hydrology.

The watershed context

The Similkameen River, nestled within its namesake watershed, is shaped by mountain hydrology typical of the region, with runoff largely influenced by snowmelt. The freshet period, which peaks from May to July, is particularly significant as it brings high water levels, replenishing the river system after winter’s snowpack has melted. This seasonal rhythm not only sustains aquatic ecosystems but also supports agricultural activities in the surrounding valley.

Why the data matters here

Today's river reading at Princeton provides insight into water conditions affecting both ecology and human activity. Measuring discharge, this station has been monitoring flows for nearly 49 years, delivering critical data to inform local usage and environmental health. Comparing today's measurement against the median for this calendar day enriches our understanding of how current conditions align with historical patterns, a more nuanced approach than evaluating raw elevation alone. The Water Survey of Canada operates this gauge, ensuring that the data reflects both natural variability and potential changes over time.

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