01/02/2021
Mapping The Ocean Bottom And Beyond
Sound can be used to map the depth of the ocean bottom. A transducer is mounted on the bottom of a ship. 🛳 Every time the transducer emits a sound, the sound travels to the ocean bottom, bounces off the bottom, and then returns to the transducer. The speed of sound in water is approximately 1500 m/s depending on the water temperature and salinity. So, we start with the simple formula of:
Speed = Change in distance / Change in time
1500 = 2 (Depth) / Change in time
Depth = 750 (Change in time)
So, the time to travel to the bottom and back tells you the depth of the ocean, at any given location, plus you must add in the distance from the transducer to the waterline of the ship. And this simple technology has been used to make detailed maps of all of the world’s oceans.