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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.
Beta. You'll be notified when a flood wave detected at an upstream gauge is forecast to reach this station, with an estimated arrival time. Accuracy improves as we verify more waves.
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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Not an emergency service — if in danger call 999. Alerts rely on
EA/SEPA/NRW data and are best-efforts. Terms
Current Level
0.449 mASD
▬ Steady
24h Max
0.449 mASD
24h Min
0.423 mASD
Typical Range
0.41 - 1.70
mASD
Highest Recorded
3.46 mASD
EA official record
3.46 in our data (since Jan 1956)
Current level is 13% of this
Current Flow
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🚽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.
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.
461 storm overflows are traced upstream of this gauge, the nearest 3.0 km away along the river. 0 report discharging now, 449 report not discharging, and for 12 the monitor is offline or has not reported, so their status is not known.
Severn Trent Water · into Tributary Of River Soar · 4.7 km away in a straight line · its watercourse is not on the river map
10 spills · 61 hours in 2025
Not discharging now · last
14 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 →
In a typical year this gauge reaches its typical high of 1.70 m
on about 44 days.
This year so far: 48 days.
202648 days, 5 of them high · 5 highso far
202536 days, 3 of them high · 3 high
202471 days, 11 of them high · 11 high
202360 days, 10 of them high · 10 high
202223 days, 2 of them high · 2 high
202140 days, 10 of them high · 10 high
202050 days, 7 of them high · 7 high
201972 days, 8 of them high · 8 high
201830 days, 1 of them high · 1 high
201716 days
Counted from each day's highest reading. Days with missing or implausible readings are left out.
The darker part is days above 2.64 m, the level this gauge tops only a few days a year.
Flood history near this gauge
Official Environment Agency warnings issued since 2006 for the 40 flood
areas linked to this gauge (nearest 0.2 km away).
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 Shardlow flood history.
Flood areas linked to this gauge
Flood warnings and alerts are issued for whole areas. These are the 40 areas linked to this gauge, nearest first.
🌊 Mixed responseA balance of quick runoff and slower groundwater baseflow.
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
0.52
mixed response
Avg Annual Rainfall
791 mm/yr
1991–2020 · +4% since 1941–70
Urban Extent
12%
partly urbanised
Median Annual Flood
257 m³/s
QMED — typical yearly peak flow
Highest Daily Mean Flow
706 m³/s
7 Nov 2000 · 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.
Sidelooker horizontal ADCP, using index velocity method to derive flows from 15/02/2008 onwards. Velocity Index gauge replaced multipath cross-configuration Ultrasonic Time of Flight gauge in 1991. Prior to 1991, gauge had a non-operational velocity-area rating which was not suitable to process flow due to being subject to variable backwater influence of the River Derwent and weed growth.
More detail
The catchment
Large catchment which contains much of Birmingham City. The Trent headwaters have small outcrops of Coal Measures whilst the Dove catchment is dominated by Millstone Grit and Carboniferous Limestone. Approx 25% of the catchment is overlain by Boulder Clay, 10% valley gravels, terraces and alluvium. Drift free areas are largely Keuper Marl and sandstone. Diverse land use from moorland to industrial.
The station
Index-Velocity station in the navigable Trent. Main channel approximately 45m wide. Gauged using ADCP boat. Station re-opened in the peak flows dataset in September 2022 (WINFAP Files v11).
How it measures flow
Originally a VA station but prone to error due to variable backwaters. Multipath cross-configuration Ultrasonic Time of Flight station installed 1991. Four major flood relief culverts on right bank and one major culvert on left bank. Velocity Index station since 2008 has been fully calibrated to highest flood flows which includes all bypass flow in a two wage index velocity equation and can be used with confidence across the full flow range from this date onwards. Original TOF gauge (1991 to 2008) did not record out of bank flows accurately as large areas of unmeasured bypass flow. Given the low frequency of such flow during the TOF gauged record an attempt was made to estimate flow at flows above bankfull. Flows are considered accurate based on extrapolation of recent high flow bypass gaugings. Early high flow current meter gaugings appear inaccurate compared to ADCP flood gaugings.
Flow regime
Very substantial flow modifications owing to imports, WRW, cooling water and industrial usage. Reservoir(s) in catchment affect runoff. Regulation from surface water and/or ground water. Runoff reduced by public water supply abstraction and increased by effluent returns. Runoff influenced by groundwater abstraction/recharge.
The flow record
Chart record commences 01/01/1955 with a complete record. Digital record commences 31/12/1982. Station could reliably be used for level only POT from 1955 to 1991, hence POT flow record commences 1991. Full period of record peak flow data reviewed and released in August 2024 (WINFAP Files v13).
Timing, not cause. Gauges can move together simply because the same rain fell on both.
Frequently asked questions
Is the River Trent at Shardlow flooding today?
The current level is 0.45m, which is within the typical range of 0.41 to 1.70m. Flooding is unlikely at this level.
Is the river level rising or falling at Shardlow?
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 Trent at Shardlow?
The typical range at this station is 0.41m to 1.70m, based on Environment Agency historical data. Levels above 1.70m 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: