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Water Level Falling Slightly
0.92

Great Haywood

Trent
Staffordshire Trent Valley catchment • Great Haywood • Staffordshire • ID: 4006 • Level
(34m ago) • 4 readings/hr • 215 views

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Current Level
0.916 mASD
▼ Falling slightly
24h Max
1.058 mASD
24h Min
0.850 mASD
Typical Range
0.80 - 1.50
mASD
Highest Recorded
3.28 mASD
EA official record
3.23 in our data (since Sep 1972)
Current level is 28% of this
🚽 Sewage overflows nearby

Recent Water Levels

🌍 floodradar.co.uk
1 day

Recent Readings

Falling · -3 cm over 5h
10 Sep 08:30 ▼ -0.1 cm 0.916 mASD
10 Sep 08:15 ▼ -0.1 cm 0.917 mASD
10 Sep 08:00 ▼ -0.2 cm 0.918 mASD
10 Sep 07:45 ▼ -0.1 cm 0.920 mASD
10 Sep 07:30 ▼ -0.1 cm 0.921 mASD
10 Sep 07:15 ▼ -0.2 cm 0.922 mASD
10 Sep 07:00 ▼ -0.1 cm 0.924 mASD
10 Sep 06:45 ▼ -0.1 cm 0.925 mASD
10 Sep 06:30 ▼ -0.2 cm 0.926 mASD
10 Sep 06:15 ▼ -0.2 cm 0.928 mASD
10 Sep 06:00 ▬ steady 0.930 mASD
10 Sep 05:45 ▼ -0.2 cm 0.930 mASD
10 Sep 05:30 ▼ -0.2 cm 0.932 mASD
10 Sep 05:15 ▼ -0.1 cm 0.934 mASD
10 Sep 05:00 ▼ -0.1 cm 0.935 mASD
10 Sep 04:45 ▼ -0.2 cm 0.936 mASD
10 Sep 04:30 ▼ -0.2 cm 0.938 mASD
10 Sep 04:15 ▼ -0.1 cm 0.940 mASD
10 Sep 04:00 ▼ -0.2 cm 0.941 mASD
10 Sep 03:45 0.943 mASD

Rainfall & Weather

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Flood history near this gauge

Official Environment Agency warnings issued since 2006 for the 14 flood areas linked to this gauge (nearest 0.9 km away).

107flood warnings 192flood alerts

Most recent flood warning: 28 Feb 2026River Blithe from Blithfield Reservoir to Bancroft

Year by year
YearWarningsAlerts
2026 3 13
2025 6 15
2024 29 25
2023 11 17
2022 2 7
2021 8 9
2020 9 15
2019 9 19
2018 1 4
2017 0 1
2016 2 9
2015 0 1
2014 0 3
2013 5 5
2012 18 22
2010 0 5
2009 1 1
2008 3 11
2007 0 8
2006 0 2

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 Great Haywood flood history.

Nearby Stations

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Station Details

  • Monitoring Station: Great Haywood
  • Watercourse: River Trent
  • Nearest Town: Great Haywood
  • County: Staffordshire
  • Nearest reservoir: Blithfield (6.8 km) · 100.0% full (as of 3 Sep 2026)
  • Coordinates: 52°48'19"N 2°0'40"W (52.805262, -2.011076)
  • Open in: Google Maps · Apple Maps (opens your maps app)
  • Date Opened: 1 Sep 1972
  • Status: Active
  • Station Type: River level station
  • Station Reference: 4006
  • EA Gauge ID: 4006-level-stage-i-15_min-mASD
  • Parameter: Level
  • Unit: mASD
  • Typical rise rate: 3 cm/hr (p95 sustained over 90 days)
  • Typical data delay: ~22 min (measured reading→publication lag)
  • Tidal: No
  • Lock / structure: No
  • Catchment Area: Staffordshire Trent Valley
  • Typical Range: 0.803 – 1.502 mASD
  • Drainage Area: 325 km² upstream of this gauge
  • EA Cross-check: 0.92 mASD (EA at 10 Sep 08:15)
  • Flow Archive: National River Flow Archive ↗

Geographic coordinates may reflect the access point for the gauge, and not the precise location in the watercourse that it is taking readings from.

Catchment Character

🌊 Fairly flashy Responds 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
0.47
mixed response
Avg Annual Rainfall
847 mm/yr
1991–2020 · +5% since 1941–70
Urban Extent
14%
partly urbanised
Highest Daily Mean Flow
42.48 m³/s
5 Dec 1960 · daily mean, not the instantaneous peak
Flow-Duration Curve
mean 4.4510.423.402.145% (high)% of days exceeded95% (low)
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.
Land Cover (2023)
Woodland 7%Grassland 55%Arable 11%Urban 26%Other 1%
Urban 23% → 26% since 1990

Flow affected by: surface-water abstraction, groundwater abstraction, effluent returns.

Photos

Gauging-station photographs from the National River Flow Archive (UKCEH).

Photos © NRFA / UKCEH & the measuring authority — shown at web resolution. Full gallery on the NRFA ↗

About this gauge

Velocity area station with broad floodplain with runoff affected by reservoirs, effluent returns and groundwater abstraction/recharge.

More detail

The catchment

Moderate catchment relief, significant urban fraction in upper catchment (Stoke-on-Trent and Newcastle-under-Lyme). Keuper Marl. Rural except for Potteries.

The station

Velocity area station with broad floodplain. Removed from peak flows dataset in May 2016 (WINFAP Files v4).

How it measures flow

High flows measured by current meter from bridge - all flows contained through bridge. Station suffers from a shifting downstream control and bed movements have rendered the site unsuitable for the processing of flows in recent years, with lots of variation evident in the gaugings taken. The station has a broad floodplain on the left bank and out of bank flows occur readily. A canal aqueduct downstream of the site may control flood levels and flows. Wide scatter is evident in spot gaugings at all levels.

Flow regime

Reservoir(s) in catchment affect runoff. Runoff influenced by groundwater abstraction/recharge. Runoff increased by effluent returns.

Descriptions from the National River Flow Archive (UKCEH). NRFA station record ↗

Gauge Details

How this gauging station is built and how long it has measured (NRFA / UKCEH).

Gauge type
Velocity–area
Operating since
1955–1964
Station datum
69.5 mAOD
Flow record
1957–1964 · 7 yrs · 100% complete
Hydrometric area
28
Measured by
Environment Agency

Frequently asked questions

Is the River Trent at Great Haywood flooding today?

The current level is 0.92m, which is within the typical range of 0.80 to 1.50m. Flooding is unlikely at this level.

Is the river level rising or falling at Great Haywood?

Based on the most recent readings, the level is currently falling slightly. The chart above shows the last 12 hours of measurements by default (up to 7 days), updated roughly every 15 minutes.

Why is the level slowly falling?

When little or no rain has fallen for a while, a river level gradually drops as the water stored in the ground and soil drains away with nothing to replace it. This is called baseflow recession and is normal in dry spells. A gentle decline like this is expected and is not a sign of a problem — downstream gauges often recede a little faster than headwaters further upstream, and levels recover once rain returns.

What is a normal level for the River Trent at Great Haywood?

The typical range at this station is 0.80m to 1.50m, based on Environment Agency historical data. Levels above 1.50m are higher than usually seen and may indicate a flood risk.

How often is this river level data updated?

Readings are taken by the Environment Agency gauge roughly every 15 minutes and FloodRadar refreshes its data continuously, so the level shown is normally less than an hour old.

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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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🏠 Buying or renting around here? Get the Property Flood-Risk Report for any English postcode — official risk band, recorded floods, warning history, river behaviour and nearby storm overflows. £19 one-off. Learn more →