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History of Oceanography
Oceanography during the World Wars
 
More of This Oceanography Feature
Part I Early Oceanography
Part 2 Oceanography and America
Part 3 Oceanography and the World Wars
Part 4 Modern Oceanography
Oceanography on the Web
Other Nautical Inventions
Oceanography Society
The World-Wide Web Virtual Library: Oceanograph
Tidal Plants
At the turn of this century, lead line soundings still remained the best method for plumbing the depth of the ocean bottom. With the coming of the First World War, however, and the widespread appearance of submarines in naval warfare for the first time, underwater sound became the technology of choice for detecting submerged targets, and sonar was born. After the War, the sonic depth finder, which determines water depths by measuring the time it takes for a pulse of sound to reach the bottom and return, was invented, and acoustic measuring techniques soon revolutionized bathymetry, the science of deep ocean depth measurements. Suddenly, the common impression that the sea floor was a flat and featureless plain changed dramatically. The bottom of the ocean turned out to be as diversified as the surface of the continents. Huge mountainous areas, volcanic cones, canyons that dwarf the Grand Canyon, and abyssal plains - all were found with the new technology. Now, any ship equipped with a depth finder could crisscross the ocean taking soundings, and contour profiles of the undersea terrain could be produced. The first bathymetric charts based on sonic soundings appeared in 1923, and they were produced regularly thereafter as new information was collected and processed.

Between the World Wars, in the 1920s and 1930s, scientific understanding of the behavior of sound in the sea and its application to sonar systems for anti-submarine warfare advanced slowly, and it was only with the emergence of a vastly increased submarine threat at the onset of the Second World War in 1939 that a major national effort was undertaken for the study of underwater acoustics. What emerged was a series of results that showed that the transmission of sound in the sea - and in particular how effectively it could be used to detect submarines - depended crucially on how the temperature and salinity of the seawater varied with depth. It was found that sound rays bend underwater in ways that are intimately linked to the variation of the speed of sound from place to place, and that this could create "shadow zones" in which a target could hide. These discoveries, and the wartime need to apply them to improving our defenses against enemy submarines, significantly widened the range of oceanic phenomena of interest to Naval Oceanographers. In addition to our traditional concerns with water depth, winds, and currents, the need to measure and interpret underwater physical parameters such as water temperature, salinity, and sound speed at increasing depths, assumed major importance. This required the development of new kinds of instruments, new analysis techniques, new ways of looking at data, and in general, a substantial broadening of the scientific disciplines needed in the practice of oceanography for naval applications.

OCEANOGRAPHY AFTER WORLD WAR II

To maintain the scientific momentum created by World War II, the Office of Naval Research was established soon after the war. Through them, private and academic oceanographic institutions began receiving funding support to continue their wartime work, and ships and other specialized platforms for conducting ocean science programs were provided. These efforts were given added impetus by the onset of the Cold War and the appearance of a significant submarine threat from the Soviet Union, including both attack submarines that could launch anti-ship cruise missiles and ballistic missile submarines off our own coasts.

Simultaneously, because the importance of accurate short-term weather forecasts had become apparent during the war, a new emphasis was placed on expanding the meteorological sciences and their applications to naval warfare. Eventually, the Naval Weather Service, established during the First World War to support naval aviation, was consolidated within the Naval Oceanography community. Therefore, we now also hold responsibility within the Navy and Marine Corps for predicting atmospheric influences on ships, aircraft, and weapon systems and providing on-scene weather forecasting to warfighting commanders at sea and on land.

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©Mary Bellis


 

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