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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.

Bradley R near Tidewater near Homer AK Water Level

Live river level, flow, historical records and forecast for Bradley R near Tidewater near Homer AK in AK, United States, built from official government gauge data.

About Bradley R near Tidewater near Homer AK

Bradley River - A vital connection to the lower Kenai Peninsula.

Nestled in the heart of Alaska's lower Kenai Peninsula, the Bradley River serves as an essential waterway for the region. Known for its dynamic flow patterns influenced by the unique subarctic hydrology, this river is a vital part of the local environment, supporting both wildlife and human activities.

The watershed context

The Bradley River flows near Tidewater, reflecting the strong connection between its waters and the surrounding landscape. As a tributary of the intricate network of rivers and streams in the Lower Kenai Peninsula, it shares its watershed with peers such as the Anchor River and the Kasilof River. While the station's drainage area is not specified, the relationship between the Bradley River and its peers underscores its role in the broader hydrological system. This region experiences a seasonal rhythm where spring breakup and snowmelt drive the annual flood cycle, often accompanied by ice jams. The warm summer months may lead to peak flows, while winter brings low flows as ice covers the river's surface.

Why the data matters here

The current measurements at the Bradley River station, operated by the U.S. Geological Survey, provide crucial insights into the river's condition. Understanding the flow patterns and water levels is essential not only for local anglers and cottagers but also for farmers and others who rely on predictable water availability. Today's reading can be compared to the median for this calendar day over a 43-year historical record, allowing for a clearer understanding of trends and anomalies within the river's flow. Such comparisons are vital, as they take into account the variability of water levels and provide a more comprehensive picture than mere elevation, aiding local residents and decision-makers in their water management endeavors.

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