Using sound to see through the sea
It’s
all about the waves

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.