Oceans - Common Questions

Science Centres: Oceans

Rob Bell's analysis of the tsunami signature.

Life cycle of an iceberg
Icebergs are biggest when they calve from the ice shelf. After that, the sun and the ocean start to melt the iceberg. Waves erode its sides and small pieces of ice constantly break off. But perhaps the most dramatic way that icebergs get smaller is by splitting, from waves flexing the iceberg, or losing their rams. Rams are portions of an iceberg that jut out horizontally from an iceberg underwater. These can break away and surge to the surface under their own buoyancy. An iceberg’s route is determined by the action of wind, waves, and ocean currents.

Ocean acidification is the name given to the lowering of pH of the oceans as a result of increasing carbon dioxide (CO2) in the atmosphere. The pH of the ocean is determined by the level of hydrogen protons (H+) in sea water. The lower the pH, the more acidic the ocean.

RV Tangaroa’s multibeam system uses a fan of sound beams to build up a 3-D picture of the seafloor (Erika Mackay)
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.