Ballon-sonde

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Ballon-sonde (sounding balloon) was the international name for weather balloons used by meteorologists to collect data from the atmosphere. These could rise to high altitudes, with the air inside expanding at lower pressure, until they burst, at which time they would fall and their measurements could be retrieved.

Illustration of a trial of L'Aërophile

Gustave Hermite and his assistant Georges Besançon are credited with inventing the ballon-sonde in 1891. Richard Assmann began using them in 1894, and they became a tool of choice for the International Commission for Scientific Aeronautics, established in 1896. Assmann Léon Teisserenc de Bort used ballons-sondes ("L'Aërophile" and "Cirrus", respectively) in taking measurements which led to the discovery of the tropopause and stratosphere.[1][2]

Abbott Lawrence Rotch reported making the first trial of ballons-sondes ("registration balloons") in the United States in 1904. He described them as follows:[3]

In Europe two types of these balloons have been employed recently; viz., large balloons of silk or paper and small balloons of india-rubber, all being filled with hydrogen gas. The economy and ease of inflation, with the advantage of a quick ascension tot he culminating point and restricted drift, led to the adoption in the St. Louis experiments of the latter form, devised by Dr. Assmann, director of the Royal Prussian Aeronautical Observatory, and made by the Continental Caoutchouc and Gutta Percha Company of Hanover, Germany. The balloons used had an initial diameter of approximately six feet when inflated with about 100 feet [sic] cubic feet of hydrogen gas, and carrying parachute and instrument exerted a net lift of nearly two pounds, which is sufficient. Being closed at the mouth they rise at an almost uniform rate of speed, expanding meanwhile until they burst at a height which is dependent upon their initial distension. A parachute, covering the top of the balloon, moderates the fall and it reaches the ground comparatively near the point of departure. The times at which the balloon left the ground and returned to it being automatically recorded and these places being known, the average direction and velocity of the balloon can be calculated, although its velocity is usually greater over the upper portion of tis course. In some cases, two balloons, unequally filled and coupled tandem, are employed, and, as only one balloon bursts, the other is borne slowly to the ground, where it continues to float and serves to attract persons to the spot. If the balloons are not badly torn they may be mended and used again, but, since the rubber has been permanently stretched, its elasticity is impaired and consequently the balloons will not rise as high as before.

A variation uses two balloons, one of which is allowed to burst, so that the apparatus makes a slow descent.[4]

In later English usage, a balloon used (with the aid of a stopwatch) to find the altitude of clouds is called a ceiling balloon, and one used to find wind velocity is called a pilot balloon.[5]

References

  1. Michel J. Rochas, "L'invention de la stratosphère", La Météorologie No. 82, August 2013.
  2. Klaus P. Hoinka, "The tropopause: discovery, definition and demarcation", Meteorol. Zeitschrift, N.F. 6, December 1997.
  3. Abbott Lawrence Rotch, "On the First Observations with Registration Balloons in America", Proceedings of the American Academy of Arts and Sciences, Vol. 41, No. 14.
  4. Shaw, 1926, Manual of Meteorology, vol. 1, pp. 224–225.
  5. Jordanoff's Illustrated Aviation Dictionary, 1942, #282 & #285, p. 57.
Enclosing categories Balloon
Subcategories
Keywords LTA, Meteo, Elasticity
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