Radio-Acoustic-Ranging
(RAR) navigation, developed within the United States Coast and
Geodetic Survey, was the very first navigation system to divorce
itself from the necessity to visually see either fixed known
objects on land for inshore piloting navigation or astronomic
bodies for celestial navigation. As such, it was the revolutionary
first step on the 70-year road that has culminated in the development
and widespread use of the Global Positioning System for land,
sea, air, and near-Earth space navigation.

First
discoveries of PIONEER and GUIDE Seamounts. Seamounts
discovered by PIONEER and GUIDE.
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RAR, like
many other technological advances in the marine sciences, had
its roots in the sinking of the TITANIC. The invention by Reginald
Fessenden of a means to transmit and receive sound waves in
the sea was the seed that led to the invention of depth-finding
sonars and other types of sonars for looking ahead of a vessel
and out to the sides of a vessel. World War I gave impetus to
this field of endeavor as German submarines were prowling shipping
lanes and sinking American and British shipping at an alarming
rate. It was imperative to devise means to discover these menaces
and take action to destroy them.
As part
of this effort, Commander Nicholas Heck of the Coast and Geodetic
Survey was attached to a Coast Artillery Unit in the New York
area that was engaged in conducting various experiments utilizing
underwater sound for the discovery of undersea objects. Heck,
who was the leader in the evolution of wiredrag and wiresweep
technology, quickly grasped the power of sonar as an underwater
search tool. But additionally, because his background involved
the precision navigation of surveying vessels, he saw the possibility
of determining the ranges of a sound source from two or more
fixed listening devices and fixing the position of that sound
source. This was the principle which developed into the RAR
method of navigation. The method devised for RAR navigation
was to drop a TNT bomb off the stern of the surveying vessel
and listen for its explosion at the ship and at two or more
fixed hydrophone locations. When the fixed hydrophones received
the signal from the explosion, this activated a radio transmitter
that would immediately transmit the reception of the signal
back to the surveying vessel. Given the distances involved,
anywhere from a few miles out to 200 miles, radio transmission
time was considered instantaneous. Thus by knowing the time
of the explosion at the ship and comparing it to time of radio
signal reception from a fixed hydrophone, the travel time of
the sound wave from explosion to the fixed hydrophone could
be determined. With knowledge of the velocity of sound in the
surrounding seawater, wave travel time multiplied by velocity
of sound in seawater would give the distance. The intersection
of two or more distances (ranges) would fix the position of
the surveying vessel at the time of the explosion. This method
was first used in 1924 by the Coast and Geodetic Survey Ship
GUIDE off the coast of Oregon.
After the
initial tests, Heck turned further development of the method
over to Robert F. Luce, the commanding officer of the GUIDE.
Within two years, RAR reception had extended 206 miles offshore
giving the first inkling of the SOFAR layer. RAR as a system
was a step in the development of: 1) radionavigation systems;
2) automated offshore telemetering buoys for oceanographic and
meteorological studies; 3) further refinement in the understanding
of the sound velocity structure of the ocean; and 4) seismic
reflection and refraction profiling.
As a navigation
method, it was used until the early years of the Second World
War when it was superceded by pure radio-navigation methods
devised to navigate both Allied and Axis bombers. The 30 photos
and diagrams in the Radio-Acoustic-Ranging section of the Coast
and Geodetic Survey album commemorate this first non-visual
navigation system. RAR should be remembered as a major step
forward in the development of electronic navigation systems,
as a forerunner of many modern oceanographic telemetering systems,
and as a stepping-stone on the path to marine seismic surveys.