At 7:15pm, Sunday 17th November GMT
Within the usual range for this location
Steady, no change from previous measurement at 7:00pm, Sunday 17th November GMT
Warning: This data is stale! For some reason, we have not been able to obtain updated levels for over 24 hours. The current displayed level is probably incorrect and you should not rely on it.
The upper Stour and surrounding tributaries
No current or recent warnings.
The River Stour from downstream of Kedington to Sudbury
No current or recent warnings.
Darker blue shaded areas on long term data indicate maximum and minimum levels for the date (you may need to zoom in closer to see them).
Long term data may have gaps where the API data was not available.
Download long term data as csvNote: CSV data will include any outlying values that have been ignored by our graphing system as probably erroneous (eg, because they are ridiculously high compared to the values either side of them). It is your responsibility to filter these out if necessary.
Important! If you are planning to retrieve the csv data automatically, you must read and understand the limitations on the data and its availability.
Please note: Geographic coordinates may reflect the access point for the gauge, and not the precise location in the watercourse that it is taking readings from.
The usual range of the Chad Brook at Long Melford is between 0.05m and 0.72m. It has been between these levels for 90% of the time since monitoring began.
The typical recent level of the Chad Brook at Long Melford over the past 12 months has been between 0.17m and 0.40m. It has been between these levels for at least 154 days in the past year.
The highest level ever recorded at the Chad Brook at Long Melford is 0.95m, reached on Sunday 22nd December 2002 at 6:00pm.
Note that this data may not take account of recent measurements, as we wait until a level has been verified by the Environment Agency before adding it to our records.
There are no other monitoring stations on the Chad Brook
Monitoring locations on nearby rivers
