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How do we map the seafloor?

Multibeam or ‘swath’ system

Multibeam echo sounders emit a fan of sound beams to the seafloor to scan a wide swath of the seabed in great detail. Compared with conventional echo sounders – which direct a single beam of sound to the seabed directly below a ship – multibeams show more detail and greatly reduce ship survey time and cost. 

A video explaining how the multibeam system on the R.V. Tangaroa works and is used can be watched at the bottom of this page, or in our video gallery.

Go to our video gallery

How it works

The hull-mounted multibeam transceiver sends out a beam of sound waves (see diagram at right) which are reflected off the seafloor, back to a receiver on the ship.

In Tangaroa’s Kongsberg EM302 multibeam system, the signal is divided into 288 separate beams, which form a swath on the seafloor. The swath width increases with water depth to a maximum of seven kilometres at a depth of about 2500 metres. It can map the seafloor at depths of up to 8000 metres.

Find out more about the Kongsberg EM302 multibeam system

We also use a portable high-resolution shallow water multibeam system (Kongsberg EM3002D). This uses the same technique but with 508 beams, very high resolution, and a range of about 1–200 m.

Building a 3-D picture of the seafloor

The multibeam system calculates water depth from the time it takes the sound to travel to the seafloor and back to the ship.

Seafloor substrate hardness and texture are indicated by the strength of the return echoes (‘backscatter’). For instance, weak echoes often indicate soft mud; strong echoes indicate rocks.

Sophisticated software combines these data with precise location data from satellite-based Differential Global Positioning Systems (DGPS) to produce various pictures of the seafloor, including:

  • charts of water depth (‘bathymetry’) as contours or colour-coded charts
  • digital elevation models – a colour-shaded relief model of the seafloor, like an aerial photograph
  • geo-referenced maps of seafloor habitats and substrates.

Preliminary charts can be plotted onboard within hours, allowing scientists to direct further survey work to areas of particular interest. These images give unprecedented insight into the intricate shape of the seafloor and the processes that shape it.

Applications include:

  • geological, oceanographic, and natural hazards research
  • marine habitat mapping
  • hydrocarbon exploration
  • seafloor engineering (including routing communications cables and pipelines)
  • managing fisheries, natural hazards, and marine protected areas. 

Further information

Technical info on Tangaroa’s EM302 multibeam system

Article about applications: ‘Managing the seabed with multibeam mapping’

Using side-scan sonar to map the seafloor under mussel farms

 

Multibeam_0.jpg

Property of NIWA LTD 2005 all rights reserved (reference 11-20859.tif).

NZBathy_EEZ_image.jpg

Annotated NZ 250m gridded bathymetric imagery, CANZ (2008) with either undersea feature names or (Exclusive Economic Zone) EEZ. An exclusive economic zone (EEZ) is a marine area prescribed by the United Nations Convention on the Law of the Sea over which a state has special rights over the exploration and use of marine resources, including energy production from water and wind.