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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.

Glacier C at Alyeska Highway at Girdwood Water Level

Live river level, flow, historical records and forecast for Glacier C at Alyeska Highway at Girdwood in AK, United States, built from official government gauge data.

About Glacier C at Alyeska Highway at Girdwood

Glacier Creek - A vital tributary of the Upper Kenai Peninsula.

Glacier Creek flows gracefully alongside the Alyeska Highway at Girdwood, Alaska, weaving through the stunning landscape of the Upper Kenai Peninsula. This waterway plays a crucial role in the regional ecosystem, offering habitat for a diverse array of wildlife and contributing to the vibrant hydrology of its surroundings.

The watershed context

Draining roughly 44 square miles, Glacier Creek captures the influx of melting snow and seasonal rains as it navigates its way through the mountainous terrain. The creek is part of a network of waterways, with neighboring peers such as the Cooper Creek near Cooper Landing and the Kenai River flowing towards Soldotna. Each of these waterways interacts within the dynamic hydrology of the Upper Kenai Peninsula, influenced by the shift of seasons that characterizes this subarctic region. Spring breakup and snowmelt drive annual flow patterns, creating opportunities for increased water levels and potential flooding, often exacerbated by ice jams.

Why the data matters here

Today's reading from the U.S. Geological Survey at Glacier Creek provides a key insight into current conditions, measured against the historical median for this date over the past nine years. The importance of comparing today's reading to the median lies in understanding fluctuations that can result from seasonal snowmelt and rain events, which are characteristic of this subarctic environment. Such data allows cottagers, anglers, and flood-watchers to make informed decisions about activities along this creek and to monitor the creek’s performance in relation to its historical context.

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