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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.

Last Mountain Lake Water Level

Live lake level, flow, historical records and forecast for Last Mountain Lake in Canada, SK, Canada, built from official government gauge data.

About Last Mountain Lake

Last Mountain Lake - A significant water body within the Last Mountain watershed.

Last Mountain Lake, located in Saskatchewan, is a prominent feature of the Last Mountain watershed, extending across an area of approximately 14,400 square kilometers. This lake plays a vital role in the local hydrology, providing essential water resources to the region and supporting the surrounding environment.

The watershed context

The Last Mountain watershed is characterized by its snowmelt-dominated hydrology, typical of the Prairie region. Spring usually sees a sharp peak in water levels, driven primarily by melting snow, which can lead to significant inflows into the lake. Following this peak, the summer months generally bring a prolonged recession in water levels as evaporation takes its toll, and inflows diminish. These seasonal patterns shape the dynamics of Last Mountain Lake, influencing its ecology and the activities of those who rely on its waters.

Why the data matters here

Today's readings from the gauge at Last Mountain Lake, registered by Water Survey of Canada, provide essential insights into the lake's current conditions. It is important to compare today's elevation against the median for this calendar day from the station's historical record of over 50 years. This context offers a clearer understanding of the water level's significance, aiding cottagers, fishermen, and anyone monitoring the lake's behavior. Such comparisons are crucial, as they reflect not only the present conditions but also help indicate trends that may impact the local environment and recreational activities.

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