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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.

Cheakamus River above Millar Creek Water Level

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

About Cheakamus River above Millar Creek

Cheakamus River above Millar Creek - A dynamic river shaped by seasonal flows.

Nestled in British Columbia's rugged landscapes, the Cheakamus River above Millar Creek flows through a watershed characterized by mountain hydrology. As part of the Strait of Georgia - Squamish watershed, this stretch of the Cheakamus River plays an important role in the local ecosystem and hydrological dynamics, especially during the freshet driven by melting snowpack. Typically, the highest flows are observed from May to July, making this a period of significant activity for both the river and the surrounding flora and fauna.

The watershed context

Draining roughly 297 square kilometers above the station, the Cheakamus River travels through a complex web of tributaries and creeks, contributing to its diverse ecological and hydrological attributes. The river is flanked by a variety of peers, including the Capilano River and Mamquam River, each with its own distinct character. The region is shaped by its mountain topography which influences rainfall patterns and streamflows, especially in summer when high-elevation areas maintain consistent water levels due to glacier-fed inputs. The Cheakamus serves as an essential conduit within this environment, supporting wildlife and providing anglers with a unique fishing experience.

This section of the river, measured by the monitoring station, also has the capacity to record discharge, complementing the elevation data and giving a fuller picture of the hydrological dynamics at play. As a living system, the Cheakamus River above Millar Creek adapts to seasonal rhythms, oscillating between high and low flows that reflect changes in both precipitation and snowmelt.

Why the data matters here

Currently, flow data from Water Survey of Canada at the Cheakamus River above Millar Creek is tracked against historical readings, providing vital context. Comparing the current reading to the median for today reveals how seasonal conditions are unfolding in relation to long-term phenomena. This perspective is crucial for a variety of stakeholders, including cottagers, anglers, and flood-watchers, who rely on accurate information to make informed decisions based on river conditions. With over 43 years of record-keeping, this data contributes significantly to understanding the ongoing changes in river health and management strategies in 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