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Understanding the downstream effects on River Thames water levels caused by Taplow Gate adjustments

Posted on January 27, 2026January 29, 2026 by ecwlarcombe

Today the River Thames is rising and the Taplow flow control structure on the Jubilee River is being operated to divert flood water away from Windsor, Eton and Maidenhead.  These actions affect water levels downstream.  Today’s date happens to be 27/1/2026 and below is a record (a snapshot) of the graphical detail available at that time.  Please note that if you follow the links below – the graphs will be different because time has moved on.

THE TAPLOW GAUGE

You will find that the gate movements at Taplow appear on the graph here

Please note that the gauge is upstream of the Taplow gates therefore the level drops as the gates are opened – and rises as the gates are closed.  The effect on the graph height appears small but the change in increased (or reduced) volume conveyed can be large.  Below records two gate openings followed by gate closure two days later.


The diverted flood water travels relatively quickly down the Jubilee River (because the channel is shorter, steeper and smoother) and re-enters the River Thames at the confluence in Datchet.


WINDSOR PARK

The Windsor Park gauge is located on the North bank of the Thames between the Windsor Road bridge and Datchet riverfront.

You will find that the gate movements at Taplow appear as definite ‘S shaped water level shocks’ on the Windsor Park graph here.

Finally – it is interesting to note that Taplow flow adjustments are also reflected on the Boulter’s Lock (downstream) and Maidenhead gauges.  I have no doubt that operation of the Taplow flow control structure (i.e. gate adjustments) introduces water flow and level disruptions that are detectable and measurable a short distance upstream and many miles downstream.


 

1 thought on “Understanding the downstream effects on River Thames water levels caused by Taplow Gate adjustments”

  1. Ian Thompson says:
    January 28, 2026 at 10:59 am

    Thank you for providing the information regarding telemetry in a way that the public may understand without complexity . Currently the River Thames is in a rising mode 28th Jan 26 , but within the normal range band . It is projected to rise just above this, dependent on expected rainfall within the coming days.

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DATCHET

The name "Datchet" is thought to be Celtic in origin, and the last part may be related to cet ("wood"). In the Domesday Book it is called "Daceta".lla. Datchet is first mentioned between 990 and 994, when King Ethelred made small grants of land here.

HORTON

The village name "Horton" is a common one in England. It is Old English in origin and derives from the two words horu 'dirt' and tūn 'settlement, farm, estate', presumably meaning 'farm on muddy soil'.In the Domesday Book of 1086 it was recorded as Hortune.

WRAYSBURY

The village name was traditionally spelt Wyrardisbury; it is Anglo Saxon in origin and means 'Wïgrǣd's fort'. Its name is recorded in the Domesday Book of 1086 as Wirecesberie and as Wiredesbur in 1195. The name is seen again as Wyrardesbury in 1422.

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