Munk had a history of collaboration with the US Navy. He spent World War II using analog methods to track waves and aid in weather predictions before
Allied amphibious landings, notably forecasting a break in an Atlantic storm that allowed Allied forces to land at Normandy on
D day in 1944. After the war, Munk remained a contractor of the Navy and continued to conduct research on its behalf throughout the
Cold War, developing a method for using low-frequency sound waves to map the ocean floor called
ocean acoustic tomography. After being asked by the US Department of Energy to forecast the effects of carbon dioxide production on the warming of the Earth, Munk faced the challenge of measuring the Earth's temperature scientifically. Although he concluded that measuring the ocean's temperature would be an excellent starting point, he still faced the issue of myriad variations across the oceans, such as differences in salinity, seasons, weather phenomena, and geography, which would make ascertaining one overall measurement very difficult. To remedy this he devised a system in which low-frequency, acoustic signals would be transmitted and recorded across vast oceanic distances. Because the speed of sound in saltwater varies based on the temperature of the water, the time it took for a transmission to reach a receiver could be converted into an ocean-wide temperature measurement. == Preparation ==