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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.

Kenai R at Soldotna AK Water Level

Live river level, flow, historical records and forecast for Kenai R at Soldotna AK in AK, United States, built from official government gauge data.

About Kenai R at Soldotna AK

Kenai River at Soldotna AK - A vibrant artery through the Upper Kenai Peninsula.

The Kenai River at Soldotna is a significant waterway flowing through Alaska's Upper Kenai Peninsula. This section of the river plays a pivotal role in the region's ecology and economy, supporting both abundant wildlife and recreational activities. Its scenic banks draw anglers, paddlers, and outdoor enthusiasts, making it a hub of activity in both summer and winter.

The watershed context

Draining roughly 2,020 square miles, the Kenai River in this reach is fed by a network of tributaries, including noteworthy peers such as the Cooper Creek and Glacier Creek. The river’s course is influenced by the unique climatic conditions of the subarctic region, where spring breakup and snowmelt initiate the annual flood cycle. This natural rhythm can create challenges, including ice jams that are common occurrences during the transition from winter to spring. As summer approaches, glacier-fed rivers like the Kenai see elevated flows, peaking in mid-to-late summer. When winter sets in, the river exhibits notably low flows under a blanket of ice.

Why the data matters here

Monitoring data from the United States Geological Survey (USGS) at the Kenai River provides crucial insights into its hydrologic behavior. Specifically, this location's observations include both stage measurements and discharge levels, enabling evaluations of water flow over time. Today's river reading is essential for understanding current conditions relative to historical trends. By comparing today’s data against the median for this calendar day over the station’s history of more than 50 years, we can better assess seasonal variations and hydrological patterns. This context not only aids local fishery management and recreational planning but also supports flood risk assessments during critical spring melt periods.

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