Radio acoustic ranging (RAR), occasionally written as "radio-acoustic ranging", was a method for determining a ship's precise location at sea by detonating an explosive charge underwater near the ship, detecting the arrival of the underwater sound waves at remote locations, and radioing the time of arrival of the sound waves at the remote stations to the ship, allowing the ship's crew to use true range multilateration to determine the ship's position. Developed by the United States Coast and Geodetic Survey (USC&GS) in 1923 and 1924 for use in accurately fixing the position of survey ships during hydrographic survey operations, it was the first navigation technique in human history other than dead reckoning that did not require visual observation of a landmark, marker, light, or celestial body, and the first non-visual means to provide precise positions. First employed operationally in 1924, RAR remained in use until 1944, when new radio navigation techniques developed during World War II rendered it obsolete.
Technique
To fix their position using radio acoustic ranging, a ship's crew first ascertained the temperature and salinity of sea water in the vicinity of the ship to determine an accurate velocity of sound through the water. The crew then threw a small TNT bomb off the ship's stern. It exploded at a depth of about , and a chronograph aboard the ship automatically recorded the time the explosion was heard at the ship. The sound traveled outward from the explosion, eventually reaching hydrophones at known locations – shore stations, anchored station ships, or moored buoys – at a distance from the ship. Each hydrophone was connected to a radio transmitter that automatically sent a signal indicating the time its hydrophone detected the sound. At the distances involved – generally less than – each of these radio signals arrived at the ship at essentially the same instant that each of the remote hydrophones detected the sound of the explosion. The ship's chronograph automatically recorded the time each radio signal arrived at the ship. By subtracting the time of the explosion from the time of radio signal reception, the ship's crew could determine the length of time the sound wave required to travel from the point of the explosion to each remote hydrophone and, knowing the speed of sound in the surrounding sea water, could multiply the sound's travel time by the velocity of sound in sea water to determine the distance between the explosion and the hydrophone. By determining the distance to at least two remote hydrophones in known locations, the ship's crew could use true range multilateration to fix the ship's position.Theberge, Alfred E., "System Without Fixed Points: Development of the Radio-Acoustic Ranging Navigation Technique (Part 1)," hydro-international.com, December 2, 2009.Rude, Gilbert T., "The Modern Chart," Motor Boating, May 1935, pp. 35, 68.In deep waters, such as those that prevailed in the Pacific Ocean along the United States West Coast, the U.S. Coast and Geodetic Survey could rely upon shore stations to support RAR because the deep water allowed sound to travel to the coast. Along the U.S. East Coast, where shallower waters prevailed, sound had greater difficulty in reaching the coast, and the USC&GS relied more heavily on anchored station ships, and later moored buoys, to support RAR.
Chronographs recorded times to the hundredth of a second, and the crew of a ship using RAR could determine their ship's distance from the remote hydrophone stations to within , allowing them to plot their ship's position with great accuracy for the time. With sound waves traveling from the point of the explosion to the distant hydrophones at about , ships occasionally used RAR at distances of over between ship and hydrophone station, and distances of were common.
Development history Precursors RAR had its origins in a growing understanding of underwater acoustics and their practical application during the early decades of the 20th century, and developed in parallel with echo sounding. The first step took place in the early 1900s, when the Submarine Signal Company invented a submarine bell signalling device and a hydrophone that could serve as a receiver of the underwater sounds the bells generated. The crew of a ship equipped with the receiving hydrophone could plot their ship's distance from the submarine bell mechanism and plot intersecting lines from two or more bells to determine the ship's position. The bells were installed at lighthouses, aboard lightvessels, and on buoys along the coasts of North America and Europe, and receiving hydrophones were mounted aboard hundreds of ships. It was history's first practical use of acoustics in an ocean environment.
The sinking of in 1912 due to a collision with an iceberg spurred the Canadian inventor Reginald Fessenden (1866–1932) to begin work on a long-distance underwater sound transmission and reception system that could detect hazards in the path of a ship. This led to the invention of the Fessenden oscillator, an electro-acoustic transducer which by 1914 had a proven ability to transmit and receive sound at a distance of across Massachusetts Bay and to detect an iceberg ahead of a ship at a range of by bouncing sound off it and detecting the echo, as well as an occasional ability to detect the reflection of sound off the ocean bottom. Further impetus to developing practical applications of underwater acoustics came from World War I, which prompted the Royal Navy, U.S. Navy, and U.S. Army Coast Artillery Corps (CAC) to experiment with sound as a means of detecting submerged submarines. In postwar experiments, the CAC's Subaqueous Sound Ranging Section conducted experiments in shallow water in Vineyard Sound off Massachusetts in which it detonated explosive charges underwater at the ends of established baselines and measured the amount of time it took for the sound to arrive at hydrophones at the other ends of the baselines in order to establish very accurate measurements of the speed of sound through water. And in 1923, the Submarine Signal Company improved upon its underwater signaling devices by equipping them with radio transmitters that sent signals both to identify the particular device and to indicate to approaching ships that it would generate an acoustic signal at a specific time interval after it sent the radio signal, allowing ships to identify the specific navigational aid they were approaching and to take advantage of a one-way ranging capability that let their crews determine their direction and distance from the navigational aid.hydro-international.com The Discovery of Long-Distance Sound Transmission in the Ocean
Nicholas Heck Realizing the potential of these applications of acoustics to hydrographic surveying and navigation, particularly along the U.S. West Coast, where fog frequently interfered with attempts to fix ship positions accurately, Ernest Lester Jones (1876–1929), then Director of the USC&GS, in consultation with USC&GS Corps officers, decided to investigate the use of acoustics in both depth finding and navigation. Nicholas H. Heck (1882–1953), a USC&GS officer, had been assigned from 1917 to 1919 to World War I service with the U.S. Naval Reserve Force, during which he had researched the use of underwater acoustics in antisubmarine warfare. He was the obvious choice to lead the new effort.
By January 1923, the USC&GS had decided to install a Hayes sonic rangefinder – an early echo sounder – aboard the survey ship USC&GS Guide, which the USC&GS planned to commission into its fleet later that year; successful operation of the sonic rangefinder would require a precise understanding of the speed of sound through water. When Heck contacted E. A. Stephenson of the CAC to inform him of this plan and to inquire further about the Vineyard Sound experiments, Stephenson suggested that a system of hydrophones detecting the sound of underwater explosions could allow USC&GS ships to fix their position while conducting surveys. Heck agreed, but believed that existing navigation aids would not meet the needs of the USC&GS in terms of the immediacy and accuracy of position fixes.NOAA History: The Start of the Acoustic Work of the Coast and Geodetic Survey He envisioned improving on the Submarine Signal Company's system of underwater noise generators and attached radio transmitters, as well as other previous concepts, by creating what would become known as the RAR method. Like echo sounding, this method required an accurate calculation of the speed of sound through water.Anonymous, "Ocean's Depth Measured By Radio Robot," Popular Mechanics, December 1938, pp. 828-830.
Heck oversaw tests at USC&GS headquarters in Washington, D.C., that demonstrated that shipboard recording of the time of an explosion could be performed accurately enough for his concept to work. He worked with Dr. E. A. Eckhardt, a physicist, and M. Keiser, an electrical engineer, of the National Bureau of Standards to develop a hydrophone system that could automatically send a radio signal when it detected the sound of an underwater explosion. When the USC&GS commissioned Guide in 1923, Heck had her based at New London, Connecticut. Under his direction, Guide both tested her new echo sounder's ability to make accurate depth soundings and conducted RAR experiments in cooperation with the CAC. Despite many difficulties, testing of both echo sounding and RAR wrapped up successfully in November 1923.
The cruise of the Guide In late November 1923, with Heck aboard, Guide began a voyage from New London via Puerto Rico and the Panama Canal to San Diego, California, where she would be based in the future, with her route planned to take her over a wide variety of ocean depths so that she could continue to test her echo sounder. Guide made history during the voyage, becoming the first USC&GS ship to use echo sounding to measure and record the depth of the sea at points along her course; she also measured water temperatures and took water samples so that the Scripps Institution for Biological Research (now the Scripps Institution of Oceanography) at La Jolla, California, could measure salinity levels. She also compared echo sounder soundings with those made by lead lines, discovering that using a single speed of sound through water, as had been the previous practice by those conducting echo sounding experiments, yielded acoustic depth-finding results that did not match the depths found by lead lines. Before she reached San Diego in December 1923, she had accumulated much data beneficial to the study of the movement of sound waves through water and measuring their velocity under varying conditions of salinity, density, and temperature, information essential both to depth-finding and RAR.Upon arriving in California, Heck and Guide personnel in consultation with the Scripps Institution developed formulas that allowed accurate echo sounding of depths in all but the shallowest waters and installed hydrophones at La Jolla and Oceanside, California, to allow experimentation with RAR. Under Heck's direction, Guide then conducted experiments off the coast of California during the early months of 1924 that demonstrated that accurate echo sounding was possible using the new formulas. Experiments with RAR, despite initial difficulties, demonstrated that the method also was practical, although difficulty with getting some of the explosive charges to detonate hampered some of the experimental program. In April 1924, the USC&GS concluded that both echo sounding and RAR were fundamentally sound, with no foundational problems left to solve, and that all that remained necessary was continued development and refinement of both techniques during their operational use. Heck turned over continued development of echo sounding and RAR to Guide'''s commanding officer, Commander Robert Luce, and returned to his duties in Washington, D.C. Later development