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.
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Live river level, flow, historical records and forecast for Cochiti East Side Main Canal at Cochiti in NM, United States, built from official government gauge data.
Cochiti East Side Main Canal - A vital waterway for the Rio Grande-Santa Fe watershed.
The Cochiti East Side Main Canal flows through the arid landscape of New Mexico, serving as a crucial irrigation channel within the Rio Grande-Santa Fe watershed. Though not a traditional river, this canal plays an essential role in delivering water to agricultural lands, particularly in an area where water is a precious commodity.
Situated within the Rio Grande-Santa Fe watershed, the Cochiti East Side Main Canal is surrounded by a network of significant water bodies, including Cochiti Lake, Galisteo Creek, and the Santa Fe River. This canal does not have a defined parent river, but it connects closely with other tributaries that help sustain the ecological fabric of the region. High-country snowmelt drives the spring flows, while the summer months can bring monsoon storms that rapidly increase water levels, affecting nearby waterways and the habitats they support.
Monitoring the flow of the Cochiti East Side Main Canal is crucial for understanding water availability in this part of New Mexico. The U.S. Geological Survey (USGS) provides real-time data on its discharge, which is essential for farmers and residents relying on this waterway for livelihood and sustenance.
Today's gauge reading is important to consider against the median for this calendar day over the last 50 years. This comparison allows for better understanding of current water conditions relative to historical patterns, which is particularly useful in an area characterized by significant fluctuations in water levels due to the seasonal rhythm of arid Southwest hydrology.
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.