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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.

Capilano River above Eastcap Creek Water Level

Live river level, flow, historical records and forecast for Capilano River above Eastcap Creek in Canada, BC, Canada, built from official government gauge data.

About Capilano River above Eastcap Creek

Capilano River above Eastcap Creek - a dynamic mountain river influenced by seasonal snowmelt.

The Capilano River above Eastcap Creek is a vital waterway in British Columbia, characterized by its robust seasonal fluctuations driven primarily by snowpack and freshets that swell from late spring into summer. This river offers insight into the unique hydrology of the region, where meltwater feeds the river, ensuring its strength as it flows through the mountainous landscape of the Strait of Georgia – Squamish watershed.

The watershed context

Draining roughly 82 square kilometres above the station, the Capilano River serves as a significant tributary in the area. It interacts with several peers, including the Capilano River at Canyon and the Cheakamus River near Brackendale, and is part of a complex network of rivers experiencing the typical seasonal rhythms of mountain hydrology seen across British Columbia. Here, the freshet peaks occur between May and July, driving the river's flow to its annual high.

The seasonal changes in flow are not just important from a hydrological perspective; they also influence the local ecosystems and human activities. As the river rises during freshet, it supports a variety of aquatic organisms and habitats.

Why the data matters here

The station at Capilano River above Eastcap Creek provides critical data on river levels and flow rates. Today's reading, compared against the historical median for this calendar day, helps contextualize the current conditions relative to typical patterns. Given its 28 years of record, this data reflects the river's response to both seasonal transitions and broader climatic influences. Monitoring this river, managed by the Water Survey of Canada, allows for informed decision-making for cottagers, anglers, and those engaged in conservation efforts within the region.

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