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+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.
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Live river level, flow, historical records and forecast for Anderson River below Carnwath River in Canada, NT, Canada, built from official government gauge data.
Anderson River below Carnwath River - A vital waterway in the subarctic.
The Anderson River, located in the Northwest Territories, flows below the Carnwath River and plays a significant role in the regional hydrology. This stretch of the river is an essential component of the Lower Anderson watershed, which encompasses a substantial drainage area of approximately 56,400 square kilometers. The river's health is closely tied to the seasonal patterns of the subarctic, where spring breakup and snowmelt dominate the hydrological cycle.
Through the long winters, the flow in the Anderson River tends to diminish beneath a covering of ice, reflecting the area's characteristic low flows. As temperatures rise, the ice melts, and the river swells with the influx of water from snowmelt. During this time, the risk of ice-jam flooding increases, creating a dynamic and sometimes unpredictable environment. The summer months are typically brief and intense, with higher flows resulting from rapid melt events. This unique seasonal rhythm shapes the ecosystem and the communities that depend on this waterway.
The Anderson River, while not connecting to other noted rivers in the region, serves as a critical channel for the water drained from the larger catchment area into surrounding landscapes. With no direct parent river mentioned, its flows contribute significantly to the overall hydrological network of the Lower Anderson watershed, impacting local wildlife and vegetation.
Monitoring the water levels and flow of the Anderson River below Carnwath River is crucial. Today's reading provides a vital comparison to the historical median for this calendar day, covering over 42 years of data. This comparison is essential, as it provides context to current conditions and highlights fluctuations that may indicate broader environmental changes. The understanding of flow dynamics is crucial for those who rely on the river for various activities, from local wildlife observations to resource management, as provided by the Water Survey of Canada.
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.