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⤴Unusual rise — FloodRadar+Top 1% rise rate for this gauge.
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You'll be notified when this gauge is rising more than 0.10 m/hr — a sign of rapidly increasing water levels.
You'll be notified when a new storm-overflow (sewage) discharge starts within ~3 km of this gauge, based on the water companies' near-real-time feeds.
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Current Level
0.739 m
▲▼ Crested · peaked 0.75
24h Max
0.745 m
24h Min
0.408 m
Typical Range
0.31 - 4.50
m
Highest Recorded
6.32 m
EA official record
6.26 in our data (since Nov 2012)
Current level is 12% of this
🚽Sewage overflows nearby
Recent Water Levels
🌍 floodradar.co.uk
1 day
EA forecast (official)
Prediction V2
Prediction Eris
Nimbus beta
Experimental model fusing soil moisture, river flow, groundwater and catchment
character. The shaded band is its 10–90% range, widened so that about 80% of recent outcomes fall inside it.
Under evaluation — not yet promoted, so treat as a second opinion.
River Flow
90 days
Daily mean discharge (m³/s) with the daily min–max band, from the EA Hydrology API. Flow is the volume of water passing the gauge — often a more direct flood signal than level.
Flow Data: Daily mean flow (m³/s) to 8 Oct (2 days behind — the EA publishes each day's mean a day or two after it ends; unchecked, provisional)via EA Hydrology
Storm overflows whose water reaches this gauge on the mapped river network, nearest first by distance along the river. The status is each water company's monitor: it says whether an overflow is discharging, not how much or what it contains.
89 storm overflows are traced upstream of this gauge, the nearest 1.7 km away along the river. 1 reports discharging now, 85 report not discharging, and for 3 the monitor is offline or has not reported, so their status is not known.
Northumbrian Water · into Bumper Ha\ll Beck · 5.9 km away in a straight line · its watercourse is not on the river map
9 spills · 1 hours in 2025
Not discharging now · last
3 other overflows within 6 km are downstream of this gauge or on another branch of the river network, so they are not listed.
These are the water companies' monitor statuses; a spill does not by itself explain a change in the gauge level. River connections and distances are traced on OS Open Rivers (edition 2026-04), which leaves out many small channels. Explore the sewage map →
Warnings apply to a whole flood area, not necessarily this exact spot. Years before 2006 aren't covered by the EA's historic record.
See also the Low Dinsdale flood history.
Flood areas linked to this gauge
Flood warnings and alerts are issued for whole areas. These are the 9 areas linked to this gauge, nearest first.
🌊 Fairly flashyResponds fairly quickly to rain, with moderate baseflow between events.
Your catchment is all the land that drains rainfall into the river above this gauge. Its character — how
steep, wet, wooded, urban or chalky that land is — decides how fast rain here turns into a rising river. A steep, bare or clay
catchment is “flashy” (rises and falls quickly, floods easily); a flat, chalk or well-wooded one is
slow and steady. The tiles below put numbers to that; the flow-duration curve reads left-to-right
from the river’s typical high flows (Q5) down to its low flows (Q95) — a steep curve means a flashy river.
The physical character of the land that drains to this gauge, and how it shapes its flood response — from the National River Flow Archive (UKCEH).
Baseflow Index
0.37
mixed response
Avg Annual Rainfall
1,019 mm/yr
1991–2020 · -3% since 1941–70
Urban Extent
2.2%
largely rural
Median Annual Flood
410 m³/s
QMED — typical yearly peak flow
Highest Daily Mean Flow
486 m³/s
25 Sep 2012 · daily mean, not the instantaneous peak
Flow-Duration Curve
Daily flow (m³/s) exceeded each % of the time — a steep curve is flashy, a flat one is steady. Q5 high · Q50 median · Q95 low.
Velocity area station. Lowest station on the River Tees. Substantial reservoir influence on flow regime.
More detail
The catchment
Geology: mostly Carboniferous (Millstone Grit and Carb. Limestone), some Magnesian Limestone; superficial deposits of boulder clay, with peat in headwaters. Moorland and rough pasture in upper catchment, mixed agriculture in lower reaches, with some urban development. No known catchment changes.
The station
Velocity area station with 47.2m wide flat V low flow control (1:2 u/s and d//s slopes, 1:40 cross slopes) constructed in 1974. No wing walls. Originally had a natural control. Lowest station on R. Tees.
How it measures flow
River overtops banks approx. 200m u/s and flows around back of station building, but is too deep to be wade gauged. Flow spills onto the right bank at 4.6m, but bypass flow is limited as the bank steepens quickly and the flow is contained. The left bank is overtopped at around 6.17m stage, with the potential for large volumes of bypass flow for a small increase in level. Significant hysteresis; modular to 0.5m. Theoretical calibration of daily flows at low flows; calibration at medium to high flows based on current meter gauging to high stages from permanent cableway, with supplementary info from hydraulic modelling. Two peak flow ratings applied across period of record, the most recent is valid from May 1974.
Flow regime
Significant overbank storage in lower reaches can attenuate flood peaks. Substantial artificial influences on the flow regime, including seven reservoirs with total area 194.6 sq.km (15.4% of catchment), influencing floods through attenuation and storage, and low flows through regulation releases (Cow Green, and in extreme droughts by Kielder transfers), and abstractions. Significant net export of water.
The flow record
Full period of record peak flow data reviewed and released in September 2020 (WINFAP Files v9).
Timing, not cause. Gauges can move together simply because the same rain fell on both.
Frequently asked questions
Is the River Tees at Low Moor flooding today?
The current level is 0.74m, which is within the typical range of 0.31 to 4.50m. Flooding is unlikely at this level.
Is the river level rising or falling at Low Moor?
Based on the most recent readings, the level is currently steady. The chart above shows the last 12 hours of measurements by default (up to 7 days), updated roughly every 15 minutes.
What is a normal level for the River Tees at Low Moor?
The typical range at this station is 0.31m to 4.50m, based on Environment Agency historical data. Levels above 4.50m are higher than usually seen and may indicate a flood risk.
How often is this river level data updated?
Readings are supplied by the Environment Agency gauge. FloodRadar checks for updates roughly every 15 minutes; the timestamp above shows how recent the latest available reading is.
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📮 Flood risk by postcode near this gauge
Postcodes within 5 km with properties in the Environment Agency’s rivers-and-sea flood-risk bands:
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1983 Weir from L bank
1983
Gauging hut and cableway on R bank
Weir looking d/s from R bank
Weir looking d/s from R bank