Verify your email to receive alerts and history exports.
Favorites
Loading…
Notifications
No active alerts
Set an alert on any lake to get notified when levels change.
The Nibi Dispatch
Water moves. Stay ahead of it.
One email a week — freshet watches, record levels, new regions. Nothing else.
Map

Sign in

Alerts & notifications Get notified when your favorite lakes go outside normal range
Loading…
Your account Email, subscription, and account actions
Loading…
DEV ZONE

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.

Chase Creek above the Mouth Water Level

Live river level, flow, historical records and forecast for Chase Creek above the Mouth in Canada, BC, Canada, built from official government gauge data.

About Chase Creek above the Mouth

Chase Creek - A vital tributary flowing towards the South Thompson River.

Chase Creek above the Mouth branches out from the mountainous terrain of British Columbia, marking its importance as it converges into the South Thompson River. The creek serves as a significant contributor to the hydrology of the area, draining roughly 293 square kilometres above the station. Its flow is characteristic of a mountain hydrology system, heavily influenced by seasonal snowpack and runoff, with peak flows typically occurring from May to July during the freshet period.

The watershed context

Nestled within the South Thompson watershed, Chase Creek above the Mouth shares its waters with a network of nearby water bodies. Notable peers include Corning Creek near Squilax, East Canoe Creek above Dam, and the Salmon River near Salmon Arm, all of which contribute to the rich hydrological character of the region. These creeks and the South Thompson River at Chase create a dynamic ecosystem influenced by the seasonal rhythms of the British Columbia landscape, where glacier-fed systems ensure sustained water levels through the summer months.

In the context of local agriculture and outdoor activities, understanding how Chase Creek interacts with its neighbors is crucial. Water levels fluctuate, often impacted by climatic conditions, affecting both water users and the ecosystems relying on consistent water flow.

Why the data matters here

Regular monitoring, conducted by the Water Survey of Canada, provides valuable insights into the creek's behavior. This diligence reveals today's measured level in relation to the median historical levels for this date, improving our understanding of typical versus unusual conditions. This morning, the creek's reading can be assessed relative to the median for today's date over a record of 28 years. Monitoring the creek's flow is essential for managing water resources effectively in a region where seasonal fluctuations can significantly influence both the natural environment and human 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