River Stort at Clavering Water Level
Live river level, flow, historical records and forecast for River Stort at Clavering in England, United Kingdom, built from official government gauge data.
- Location England, United Kingdom
- Primary gauge ea-5112TH (Environment Agency)
About River Stort at Clavering
River Stort at Clavering is a gauged river in England.
What the record shows
This station has more than 26 years on record.
The highest level in the file is 1.44 m (4.71 ft), set in January 2026. The lowest is -0.26 m (-0.86 ft), set in February 2007. That span tells you the Stort can sit close to zero for long periods, then jump well clear of that base when conditions turn wet.
The seasonal pattern is plain. January is the highest month, with a typical level of 0.42 m (1.36 ft). September is the lowest month, with a typical level of 0.04 m (0.14 ft). The typical annual swing is 37.4 cm (14.7 in). For people using the river edge, that is the range a mooring line, bank step, or low intake has to live with over a normal year.
The watershed
No watershed name is given for this page, so the record has to be read as this reach only.
The seasonal rhythm fits temperate hydrology: higher water in the colder months and lower water toward late summer. January stands out as the usual high point, while September is the usual low. For an angler, that means the channel is often carrying more water and faster margins in winter, then easing back to its shallowest levels later in the season. For someone with equipment near the bank, the 37.4 cm (14.7 in) swing is the number to keep in mind.
Reading the hero number
The hero number compares today’s reading with the median for this calendar day across the station record. That is more useful than raw elevation because a level by itself does not show whether the river is running above or below its normal pattern for this date.
This page is based on Environment Agency records. With more than 26 years of measurements here, the day-to-day comparison gives a better read on what the river is doing now than a single height on its own.
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
Nibi Metrics - live water levels, flow, and forecasts for lakes and rivers across Canada, the US and the UK
Real-time water levels, forecasts, and alerts for lakes and rivers across Canada, the US and the UK. Built on official government data.
Nibi Metrics tracks more than 13,000 gauged lakes and rivers across Canada, the United States and the United Kingdom, reading directly from official federal monitoring networks: the Water Survey of Canada, the United States Geological Survey, Quebec's provincial hydrometric network, and the Environment Agency for England. Every number on the platform is measured, not modelled - taken from a government gauge on the water itself and compared against that location's own historical record for this exact date.
What you can see for any monitored lake or river
The level right now, in feet or metres, updated as the source agency publishes new readings - for many stations that is every five to fifteen minutes. How today compares to typical: every location carries its own typical-for-this-date band built from its historical record, so a reading is never just a number - it is above, below, or near what this water usually does on this calendar day. Which way it is moving: a measured RISING, FALLING, or STEADY verdict computed from the gauge's own recent readings, with the rate of change - the difference between a flood ending and one beginning. What comes next: level forecasts up to 72 hours ahead, driven by the gauge's recent behaviour, upstream water, and quantitative precipitation forecasts, alongside live radar, lightning, and weather for the surrounding region.
Alerts that watch the water for you
Set a threshold on any location - a level, a distance above typical, or a rate of climb - and Nibi emails or notifies you the moment the gauge crosses it. Cottagers use it for spring freshet, anglers for river conditions, marinas and municipalities for operations. The scanning runs around the clock against the same measured data shown on every page.
Where Nibi comes from
Nibi means water in Anishinaabemowin. The platform began at a family cottage on Lake Muskoka, Ontario, where the spring melt floods the shoreline most years and the only forecast was standing on the dock, looking, and guessing. It grew into an independent, member-funded platform run by Muskoka Research Inc. - no investors, no data resale, and a privacy policy shorter than most cookie banners. The core data is free for everyone, forever; paid plans add automation like multi-location alerts, deep history, and reports.
Coverage
Nibi spans the continent: every Canadian province and territory with active federal gauges - from Vancouver Island rivers to the Muskoka lakes, prairie reservoirs, and Quebec's hydrometric network - and the United States from Maine to the Texas Hill Country, the Ohio Valley, and the Pacific Northwest. Coverage grows where the water news is: when a basin floods, its gauges join the platform with their full historical records attached. Many stations report every five to fifteen minutes; most report at least hourly; every page states exactly when its gauge last spoke.
Free forever, funded by members
The core promise is simple: the water data is free, for everyone, forever. Live levels, maps, radar, and recent history never sit behind a paywall. Paid plans fund the platform by adding automation - multi-location alerts, decades of history, longer forecasts, and PDF reports - so the people who need more carry the cost for everyone who just needs to check the lake before driving up. There are no investors and no advertising deals shaping what the data says.
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How every number is computed - About the platform
