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A GPS sonde, approx 220 × 80 ×75 mm (8.7 × 3.1 × 3 in) (with grounding station in background, used to perform a 'ground check' and also recondition the humidity sensor)

A radiosonde (Sonde is French and German for probe) is a battery-powered telemetry instrument package carried into the atmosphere usually by a weather balloon that measures various atmospheric parameters and transmits them by radio to a ground receiver. Radiosondes may operate at a radio frequency of 403 MHz or 1680 MHz. A radiosonde whose position is tracked as it ascends to give wind speed and direction information is called a rawinsonde ("radar wind -sonde").[1][2] Most radiosondes have radar reflectors and are technically rawinsondes. A radiosonde that is dropped from an airplane and falls, rather than being carried by a balloon is called a dropsonde. Radiosondes are an essential source of meteorological data, and hundreds are launched all over the world daily.

Modern radiosondes measure or calculate the following variables:

Radiosondes measuring ozone concentration are known as ozonesondes.[3]


  • History 1
  • Operation 2
  • Routine radiosonde launches 3
  • Uses of upper air observations 4
  • See also 5
  • References 6
  • External links 7


Kites used to fly a meteograph
Meteograph used by the US Weather Bureau in 1898
US sailors launching a radiosonde during World War 2

The first flights of aerological instruments were done in the second half of the 19th century with kites and meteographs, a recording device measuring pressure and temperature that was recuperated after the experiment. This proved to be difficult because the kites were linked to the ground and were very difficult to manoeuvre in gusty conditions. Furthermore, the sounding was limited to low altitudes because of the link to the ground.

Trappes the first regular daily use of these balloons. Data from these launches showed that the temperature lowered with height up to a certain altitude, which varied with the season, and then stabilized above this altitude. De Bort's discovery of the tropopause and stratosphere was announced in 1902 at the French Academy of Sciences.[4] Other researchers, like Richard Aßmann and William Henry Dines, were working at the same times with similar instruments.

In 1924, Colonel William Blaire in the U.S. Signal Corps did the first primitive experiments with weather measurements from balloon, making use of the temperature dependence of radio circuits. The first true radiosonde that sent precise encoded telemetry from weather sensors was invented in France by Robert Bureau. Bureau coined the name "radiosonde" and flew the first instrument on January 7, 1929.[4][5] Developed independently a year later, Pavel Molchanov flew a radiosonde on January 30, 1930. Molchanov's design became a popular standard because of its simplicity and because it converted sensor readings to Morse code, making it easy to use without special equipment or training.[6]

Working with a modified Molchanov sonde, Sergey Vernov was the first to use radiosondes to perform cosmic ray readings at high altitude. On April 1, 1935, he took measurements up to 13.6 km (8.5 mi) using a pair of Geiger counters in an anti-coincidence circuit to avoid counting secondary ray showers.[6][7] This became an important technique in the field, and Vernov flew his radiosondes on land and sea over the next few years, measuring the radiation's latitude dependence caused by the Earth's magnetic field.

During the 1930s the expansion of economically important government weather forecasting services and their increasing need for data motivated many nations to begin regular radiosonde observation programs

In 1985, as part of the Soviet Union's Vega program, the two Venus probes, Vega 1 and Vega 2, each dropped a radiosonde into the atmosphere of Venus. The sondes were tracked for two days.

Although modern remote sensing by satellites, aircraft and ground sensors is an increasing source of atmospheric data, none of these systems can match the vertical resolution (30 m (98 ft) or less) and altitude coverage (30 km (19 mi)) of radiosonde observations, so they remain essential to modern meteorology.[1]

Although hundreds of radiosondes are launched worldwide each day year-round, the only known fatality attributed to a radiosonde was the electrocution of a lineman in the United States who was attempting to free a radiosonde from high-tension power lines in 1943.[8][9]


A rubber or latex balloon filled with either helium or hydrogen lifts the device up through the atmosphere. The maximum altitude to which the balloon ascends is determined by the diameter and thickness of the balloon. Balloon sizes can range from 100 to 3,000 g (3.5 to 105.8 oz). As the balloon ascends through the atmosphere, the pressure decreases, causing the balloon to expand. Eventually, the balloon will expand to the extent that its skin will break, terminating the ascent. An 800 g (28 oz) balloon will burst at about 21 km (13 mi).[10] After bursting, a small parachute on the radiosonde's support line carries it to Earth. A typical radiosonde flight lasts 60 to 90 minutes. One radiosonde from Clark Air Base, Philippines, reached an altitude of 155,092 ft (47,272 m).

The modern radiosonde communicates via radio with a computer that stores all the variables in real time. The first radiosondes were observed from the ground with a theodolite, and gave only a wind estimation by the position. With the advent of radar by the Signal Corps it was possible to track a radar target carried by the balloons with the SCR-658 radar. Modern radiosondes can use a variety of mechanisms for determining wind speed and direction, such as a radio direction finder or GPS. The weight of a radiosonde is typically 250 g (8.8 oz).

Sometimes radiosondes are deployed by being dropped from an aircraft instead of being carried aloft by a balloon. Radiosondes deployed in this way are called dropsondes.

Routine radiosonde launches

Worldwide there are more than 800 radiosonde launch sites. Most countries share data with the rest of the world through international agreements. Nearly all routine radiosonde launches occur 45 minutes before the official observation time of 0000 UTC and 1200 UTC, so as to provide an instantaneous snapshot of the atmosphere.[11] This is especially important for numerical modeling. In the United States the National Weather Service is tasked with providing timely upper-air observations for use in weather forecasting, severe weather watches and warnings, and atmospheric research. The National Weather Service launches radiosondes from 92 stations in North America and the Pacific Islands twice daily. It also supports the operation of 10 radiosonde sites in the Caribbean.

A list of U.S. operated land based launch sites can be found in Appendix C, U.S. Land-based Rawinsonde Stations[12] of the Federal Meteorological Handbook #3,[13] titled Rawinsonde and Pibal Observations, dated May 1997.

Uses of upper air observations

Raw upper air data is routinely ingested by numerical models. Forecasters often view the data in a graphical format, plotted on thermodynamic diagrams such as Skew-T log-P diagrams, Tephigrams, and or Stüve diagrams, all useful for the interpretation of the atmosphere's vertical thermodynamics profile of temperature and moisture as well as kinematics of vertical wind profile.

Radiosonde data is a crucially important component of numerical weather prediction. Because a sonde may drift several hundred kilometers during the 90- to 120-minute flight, there may be concern that this could introduce problems into the model initialization. However, this appears not to be so except perhaps locally in jet stream regions in the stratosphere.[14]

See also


  1. ^ a b "Frequently asked questions about NWS observation program". Upper-air observation program. US National Weather Service, National Oceanographic and Atmospheric Administration. 
  2. ^ "Rawinsonde". Encyclopaedia Britannica online. Encyclopaedia Britannica Inc. 2014. Retrieved June 15, 2014. 
  3. ^ Karin L. Gleason (March 20, 2008). "Ozonesonde". National Oceanic and Atmospheric Administration. Retrieved 2011-07-04. 
  4. ^ a b "Radiosondage". Découvrir : Mesurer l’atmosphère (in Français).  
  5. ^ "Bureau (Robert)". La météo de A à Z > Définition (in Français).  
  6. ^ a b DuBois, Multhauf and Ziegler, "The Invention and Development of the Radiosonde", Smithsonian Studies in History and Technology, No. 53, 2002.
  7. ^ Vernoff, S. "Radio-Transmission of Cosmic Ray Data from the Stratosphere", Nature, June 29, 1935.
  8. ^ "Linemen Cautioned About Disengaging Radiosonde," Electrical World, 15 May 1943
  9. ^
  10. ^ Dian J. Gaffen. Radiosonde Observations and Their Use in SPARC-Related Investigations. Retrieved on 2008-05-25.
  11. ^ Preflight Procedures and Success Criteria Archived November 21, 2008 at the Wayback Machine
  12. ^ U.S. Land-based Rawinsode Stations
  13. ^ "Federal Meteorological Handbook #3". Retrieved 2013-09-15. 
  14. ^ Dead link

External links

  • Upper air data for the world - past and present
  • WMO spreadsheet of all Upper Air stations around the world
  • Interpreting radiosonde data Tephigrams and Skew-T log P diagrams.
  • Radiosonde Sounding System at
  • NOAA National Weather Service Radiosonde Factsheet
  • Sergei Nikolaevich Vernov
  • SCR-658 pics
  • early pics
  • Photo - Early Type Radiosonde
  • Photo - Radiosonde, Transistor Type
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