Using sound to see through the sea

It’s all about the waves
Hydrography is a branch of applied science, which involves measuring the depth of water and identifying hazards that lie on the seabed.  Knowing the locations of things such as wrecks and rocks helps boats and people move safely at sea.

Normally you can’t see the seabed, so the way in which we measure the water depth is by using sound. We use a system called echo sounding. This works in a similar way to when you stand in a cave and shout out your name and hear your echo come back. The echo sounder is fitted on the bottom of the boat and ‘shouts’ at ultrasonic frequencies, and then listens for the response.

The sound of the sea
In simple terms it’s “speed = distance/time”.  The speed of sound in water is known (or can easily be calculated), and so by measuring the time it takes for the sound to return gives you the distance it has travelled to the seabed and back.
In reality it’s a bit more complicated than this as the speed of sound can vary – such as where freshwater from rivers meets the saltwater of the seas – and where the movement of the boat, tides, and the angle and type of seabed can all vary.

Using science to see clearly
However, using maths and physics, all the factors can be understood to give the super accurate answer we need of how deep the sea is. On our boats we use multi-beam echo sounders which give hundreds of readings every second.  This gives us detailed knowledge of the seabed and the chance to visualise what it looks like, just by listening to the sound waves coming back.
This is how we use the science of sound, to see through the sea.

If you want to see some of the latest data and images of the seabed around the UK, you can follow this link; www.gov.uk/guidance/inspire-portal-and-medin-bathymetry-data-archive-centre

Bob Kinnear, MCA Hydrography Manager.

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