For an event, particularly in the Indian Ocean which happens once every 60 years, you obviously cannot have a frequent real-time testing. But if you look at it as a science, you don’t need an earthquake or a tsunami of that magnitude to test the system. A system consists of various elements. In this case, we have sensors at the bottom of the ocean, various tide gauges, seismological equipment, and we are getting seismological data from across the world. Each of these individual systems is tested 24 hours. For example, we have placed the Bottom Pressure Recorders (BPR) at the depth of, say, 3km which gives a reading every hour. So we know whether the recorder is working or not. It is also highly accurate. We know how the variations take place with respect to the normal tides so we know exactly how the BPR is working because all these tides have a definite mathematical model. Similarly, the tide gauges are also tested. The seismological equipment is tested very frequently because there are so many earthquakes taking place at a low magnitude. When these work for low magnitude, they will also work for high magnitude. Most of the equipment is being tested and monitored by computers on a 24 hour basis. |