At 5:30am, Sunday 22nd December GMT
Within the usual range for this location
Rising, 0.010 from previous measurement at 5:00am, Sunday 22nd December GMT
River Windrush at Witney and Ducklington
No current or recent warnings.
River Windrush from Bourton to Newbridge
Flood Alert
River Windrush at Asthall, Minster Lovell and Crawley
No current or recent warnings.
River Thames and tributaries from Buscot Wick down to Kings Lock
Recent warnings or alerts no longer in force
Clanfield Brook for Clanfield Village and the Shill Brook for Bampton
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 River Windrush at Witney is between 0.46m and 1.40m. It has been between these levels for 90% of the time since monitoring began.
The typical recent level of the River Windrush at Witney over the past 12 months has been between 0.57m and 1.41m. It has been between these levels for at least 151 days in the past year.
The highest level ever recorded at the River Windrush at Witney is 2.45m, reached on Friday 25th December 2020 at 12:00am.
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.
Monitoring locations on nearby rivers
