FloodRadar
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Geographic coordinates may reflect the access point for the gauge, and not the precise location in the watercourse that it is taking readings from.
Gauges connected to this river, and others nearby. A distance “by river” follows the river on the map; any other is in a straight line.
Distances by river: OS Open Rivers. Contains OS data © Crown copyright and database rights 2026.
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.
31 storm overflows are traced upstream of this gauge, the nearest 8.1 km away along the river. 0 report discharging now, 31 report not discharging.
23 more further upstream, up to 66.8 km away along the river.
Within 6 km in a straight line, but the river map cannot say whether their water passes this gauge.
1 more within 6 km whose connection is not known.
8 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 2026-10), which leaves out many small channels. Sewage & storm overflows →
Contains OS data © Crown copyright and database rights 2026.
Loading rainfall and weather data...
Official Environment Agency warnings issued since 2006 for the 5 flood areas linked to this gauge (nearest 1.1 km away).
Most recent flood warning: 27 Jan 2026 — River Torridge (Lower) from Dolton to Bideford, including Taddiport and Weare Giffard
| Year | Severe | Warnings | Alerts |
|---|---|---|---|
| 2026 | 0 | 2 | 1 |
| 2025 | 0 | 5 | 8 |
| 2024 | 0 | 9 | 9 |
| 2023 | 0 | 5 | 9 |
| 2022 | 0 | 2 | 2 |
| 2021 | 0 | 4 | 8 |
| 2020 | 0 | 9 | 10 |
| 2019 | 0 | 4 | 7 |
| 2018 | 0 | 3 | 9 |
| 2017 | 0 | 0 | 3 |
| 2016 | 0 | 1 | 7 |
| 2015 | 0 | 5 | 8 |
| 2014 | 1 | 9 | 6 |
| 2013 | 0 | 5 | 12 |
| 2012 | 0 | 17 | 17 |
| 2011 | 0 | 2 | 2 |
| 2010 | 0 | 1 | 1 |
| 2009 | 0 | 3 | 7 |
| 2008 | 0 | 4 | 5 |
| 2007 | 0 | 3 | 4 |
| 2006 | 0 | 2 | 3 |
Warnings apply to a whole flood area, not necessarily this exact spot. Years before 2006 aren't covered by the EA's historic record.
Flood warnings and alerts are issued for whole areas. These are the 5 areas linked to this gauge, nearest first.
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).
Flow affected by: surface-water abstraction, reservoir influence, public water supply, effluent returns, industrial / agricultural abstraction.
Gauging-station photographs from the National River Flow Archive (UKCEH).
28 Nov 2006
13 Sep 2006 View to bed control from downstream. Low flow conditions.
13 Sep 2006 View to bed control from upstream.
6 Apr 2006 View to bed control from upstream.
6 Apr 2006 View to hut from left bank.
28 Dec 1994 Looking downstream (main channel) from road bridge.
28 Dec 1994 View down left bank overspill from road bridge. Stage = 4.3m. Water flowing over floodbank into field.
28 Dec 1994 Looking upstream from road bridge. Stage = 4.3m.
28 Dec 1994 View over hut roof across cableway section and floodplain. Stage = 4.3m.
28 Dec 1994 View down left bank overspill from road bridge. Stage = 4.3m. Cableway tower on top of flood bank can be seen in the middle ground.
31 Oct 1994 Looking down left bank overspill from road bridge.
31 Oct 1994 View downstream from road bridge. Water flowing over left bank floodbank into field. Cableway tower on top of flood bank can be seen on left hand side of picture.
Photos © NRFA / UKCEH & the measuring authority — shown at web resolution. Full gallery on the NRFA ↗
Velocity area station built in 1960 and reconstructed in 1977.
Descriptions from the National River Flow Archive (UKCEH). NRFA station record ↗
How this gauging station is built and how long it has measured (NRFA / UKCEH).
The latest recorded level is 5.54m3/s. Compare it with the recent history on the chart above to judge whether levels are unusually high.
Based on the most recent readings, the level is currently falling. The chart above shows the last 12 hours of measurements by default (up to 7 days), updated roughly every 15 minutes.
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. Only about 0.3mm of rain has fallen nearby in the last 7 days, so the flow is being sustained mainly by groundwater. 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.
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.
Free live river-level widget — ideal for parish councils, angling clubs and local sites. Updates automatically.
Postcodes within 5 km with properties in the Environment Agency’s rivers-and-sea flood-risk bands:
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