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
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.
Inside the freshet cycle that puts Manitoba shorelines at risk each year - and why 2026 broke the script.
The science of snow water equivalent and why it drives the season ahead.
What the numbers on the measuring stick actually tell you.
Why Central and South Texas rivers go from gravel beds to fifty-year records in an afternoon - including July 2026 on the Nueces.
One percent, every year, forever - unwrapping hydrology's most misunderstood phrase, and how it differs from our own percentiles.
Knik R near Palmer AK Water Level
Live river level, flow, historical records and forecast for Knik R near Palmer AK in AK, United States, built from official government gauge data.
- Location AK, United States
- Watershed matanuska
- Primary gauge 15281000 (USGS)
About Knik R near Palmer AK
Knik River - A vital waterway of the Matanuska watershed.
The Knik River near Palmer, Alaska, is a significant waterway within the Matanuska watershed. Flowing through a region shaped by subarctic conditions, the river experiences distinct seasonal rhythms influenced by snowmelt and ice dynamics. Its waters support local ecosystems and connect to other rivers, including the Matanuska River and Moose Creek, creating a network that is essential for both the local wildlife and aquatic activities.
The watershed context
The Knik River's drainage area encompasses roughly 1,220 square miles, representing the region that contributes to its flow. This expansive catchment collects melting snowpack in the spring, which leads to a pronounced annual flood event. The subarctic hydrology of Alaska brings colder winters and significant ice cover, particularly during deep winter, resulting in low flow levels until the thaw begins. Spring breakup can lead to unique challenges, including the possibility of ice jams, as the transition to warmer weather prompts rapid changes in water levels.
Why the data matters here
Current monitoring by the U.S. Geological Survey (USGS) provides insight into the river's health and flow dynamics. Water levels are tracked to give real-time data that helps assess conditions for cottagers, anglers, and those with interests in flood preparedness. Understanding today's river level in relation to historical data reveals the performance of the Knik River against its median for this date—critical information for managing activities on and around the river. This helps residents and visitors appreciate the natural ebb and flow of this essential Alaskan river.
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
