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⤴Unusual rise — FloodRadar+Top 1% rise rate for this gauge.
Height for "Above a height"
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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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Not an emergency service — if in danger call 999. Alerts rely on
EA/SEPA/NRW data and are best-efforts. Terms
Current Level
0.259 mASD
▬ Steady
24h Max
0.275 mASD
24h Min
0.253 mASD
Typical Range
0.27 - 0.75
mASD
Highest Recorded
1.56 mASD
EA official record
A 2.19 reading (20 Apr 1986) sits in our unverified raw history and is not treated as the record
Current level is 17% 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 6 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.
4 storm overflows are traced upstream of this gauge, the nearest 19.3 km away along the river. 0 report discharging now, 2 report not discharging, and for 2 the monitor is offline or has not reported, so their status is not known.
Severn Trent Water · into Tideswell Brook · 5.8 km away in a straight line · its watercourse is not on the river map
4 spills · 3 hours in 2025
Not discharging now · last
7 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 0.75 m
on about 40 days.
This year so far: 4 days.
20264 days so far
20258 days
202436 days, 2 of them high · 2 high
202347 days, 4 of them high · 4 high
202246 days, 4 of them high · 4 high
202142 days, 1 of them high · 1 high
202049 days, 3 of them high · 3 high
201960 days, 2 of them high · 2 high
201834 days, 1 of them high · 1 high
201734 days, 8 of them high · 8 high
Counted from each day's highest reading. Days with missing or implausible readings are left out.
The darker part is days above 1.54 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 14 flood
areas linked to this gauge (nearest 1.3 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 Ashford in the Water flood history.
Flood areas linked to this gauge
Flood warnings and alerts are issued for whole areas. These are the 14 areas linked to this gauge, nearest first.
🌊 Groundwater-fedSlow and steady — fed largely by groundwater, so levels change gradually, not in sudden spikes.
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
0.68
groundwater-fed — slow & steady
Avg Annual Rainfall
1,229 mm/yr
1991–2020 · +2% since 1941–70
Urban Extent
2.3%
largely rural
Median Annual Flood
16.85 m³/s
QMED — typical yearly peak flow
Highest Daily Mean Flow
30.67 m³/s
27 Oct 1998 · 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.
Open channel section until flat V weir commissioned in 1994.
More detail
The catchment
Moderate to high relief catchment in S Pennines. Carboniferous Limestone with basic sills and intrusions in upper catchment. Isolated hill top peat. Buxton in the headwaters, otherwise moorland, grazing, forested main valley.
The station
Open channel station opened 1965. Problems with severe seasonal weed growth led to closure of original velocity-area station in 1977 (telemetry of levels maintained). Flat-V weir (1:20 cross-slopes) commissioned 1994. Located just downstream of bridge in meandering reach; channel 11m wide.
How it measures flow
Open channel station well-rated to bankfull by gauging, and the December 1965 event gauged by current meter at 2.36m and 27.9 m3/s. There appears to have been a datum shift in March 1970 of around +0.30m. Applying a datum shift of +0.31m to data before 11/03/1970 and then applying the pre-weir rating gives similar flows to those shown in most cases (maximum difference of under 2 m3/s). Stage hydrographs of AMAX events in early record look reasonable. Although few gaugings above QMED pre- and post-weir, the highest events in both periods were gauged near the peaks. Most recent rating valid from April-1994 when weir installed. Pre-weir rated up to bankfull (2.35m). Post-weir rating valid to 2m; max gauging 1.55m; upper limb based on 2 gaugings. Post-weir high flows are derived from rating curve fitted to spot flow gaugings - gaugings suggest channel control at high flows is stable. Embankment limits spills onto left bank (see photos near peak of October 1998 event). Weir drowns at high flows. Weed/algae problems. Two peak flow ratings across period of record.
Flow regime
Modest net augmentation to flows from WRW and PWS.
The flow record
Low flows: Pre-weir record of limited value due to shifting bed control caused by annual weed growth. (But 1976 7-day minimum may be lower than that for 1995). No daily flows recorded 1977 to 1994. Data prior to 1965 is not held on record as deemed unreliable. Full period of record peak flow data reviewed and released in August 2025 (WINFAP Files v14).
Timing, not cause. Gauges can move together simply because the same rain fell on both.
Frequently asked questions
Is the River Wye at Ashford in the Water flooding today?
The current level is 0.26m, which is below the typical range. Flooding is very unlikely at this level.
Is the river level rising or falling at Ashford in the Water?
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 Wye at Ashford in the Water?
The typical range at this station is 0.27m to 0.75m, based on Environment Agency historical data. Levels above 0.75m 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: