WHAT'S HAPPENING NOW
+88.8 ft above typical
Finding the top signal on the water…
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.
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.
Live river level, flow, historical records and forecast for Consecon Creek at Allisonville in Canada, ON, Canada, built from official government gauge data.
Consecon Creek - A vital stream in the Prince Edward Bay watershed.
Consecon Creek flows through the scenic landscapes of Ontario, draining a catchment area of approximately 120 square kilometres. This lively watercourse is an integral part of the Prince Edward Bay watershed, contributing to the regional ecology and water dynamics. The creek's hydrology is notably influenced by seasonal changes, particularly snowmelt-driven flows that typically surge during the spring months of late April and May. As temperatures rise, the melting snow feeds the creek, resulting in increased water levels that are essential for local ecosystems and agricultural practices.
The Consecon Creek at Allisonville plays a key role within the larger framework of Prince Edward Bay. With no parent river to visibly connect to, it remains a distinct stream that draws its life from the precipitation that falls within its 120 square kilometre catchment. The watershed's seasonal rhythm marks distinct periods of activity and quiet. Following the spring freshet, a natural drawdown occurs during the summer months, lasting from July through September, when evaporation and reduced inflows cause water levels to decrease. As autumn approaches, early winter leads to an additional decline in water levels as ice begins to form, marking the transition into the winter season.
Understanding the hydrometric data for Consecon Creek is essential for local stakeholders, including farmers, cottagers, and environmental monitors. The creek's water levels can be significantly impacted by the seasonal dynamics of the region. By observing the current readings against the median for this calendar day over the past 50 years, recorded by Water Survey of Canada, we can gain valuable insights into trends and anomalies. This context is crucial for predicting changes that could affect both the human and ecological communities relying on this important waterway.
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.