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Radiosonde

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collect weather data in remote and inhospitable locations. By 1940, the NBS radiosonde system included a pressure drive, which measured temperature and humidity as functions of pressure. It also gathered data on cloud thickness and light intensity in the atmosphere. Due to this and other improvements in cost (about $ 25), weight (> 1 kilogram), and accuracy, hundreds of thousands of NBS-style radiosondes were produced nationwide for research purposes, and the apparatus was officially adopted by the U.S. Weather Bureau.
1254: 353:. 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). After bursting, a small 159: 143: 1642: 1899: 1909: 527:
Africa have experienced severe (57%) and moderate (25%) radiosonde data gap. This dire situation has prompted call for urgent need to fill the data gap in Africa and globally. The vast data gap in such a large part the global landmass, home to some of the most vulnerable societies, the aforementioned call has galvanised a global effort to “plug the data gap” in the decade ahead and halt a further deterioration in the observation networks.
28: 263:. In 1937, Diamond, along with his associates Francis Dunmore and Wilbur Hinmann, Jr., created a radiosonde that employed audio-frequency subcarrier modulation with the help of a resistance-capacity relaxation oscillator. In addition, this NBS radiosonde was capable of measuring temperature and humidity at higher altitudes than conventional radiosondes at the time due to the use of electric sensors. 170:, a recording device measuring pressure and temperature that would be recovered after the experiment. This proved 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. 396:
Radiosondes weather balloons have conventionally been used as means of measuring atmospheric profiles of humidity, temperature, pressure, wind speed and direction. High-quality, spatially and temporally “continuous” data from upper-air monitoring along with surface observations are critical bases for
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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.
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which stated that "the situation in Africa shows a dramatic decrease of almost 50% from 2015 to 2020 in the number of radiosonde flights, the most important type of surface-based observations. Reporting now has poorer geographical coverage". Over the last two decades, some 82% of the countries in
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In order to improve harmonisation in spectrum utilisation, the majority of service-allocations stipulated in this document were incorporated in national Tables of Frequency Allocations and Utilisations which is with-in the responsibility of the appropriate national administration. The allocation
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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
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Although hundreds of radiosondes are launched worldwide each day year-round, fatalities attributed to radiosondes are rare. The first known example was the electrocution of a lineman in the United States who was attempting to free a radiosonde from high-tension power lines in 1943. In 1970, an
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In 1938, Diamond developed the first ground receiver for the radiosonde, which prompted the first service use of the NBS radiosondes in the Navy. Then in 1939, Diamond and his colleagues developed a ground-based radiosonde called the “remote weather station,” which allowed them to automatically
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Lamentably, in less developed parts of the globe such as Africa, which has high vulnerability to impacts of extreme weather events and climate change, there is paucity of surface- and upper-air observations. The alarming state of the issue was highlighted in 2020 by the
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on the radiosonde's support line may slow its descent to Earth, while some rely on the aerodynamic drag of the shredded remains of the balloon, and the very light weight of the package itself. A typical radiosonde flight lasts 60 to 90 minutes. One radiosonde from
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understanding weather conditions and climate trends and providing weather and climate information for the welfare of societies. Reliable and timely information underpin society’s preparedness to extreme weather conditions and to changing climate patterns.
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in an anti-coincidence circuit to avoid counting secondary ray showers. 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
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Worldwide, there are about 1,300 radiosonde launch sites. Most countries share data with the rest of the world through international agreements. Nearly all routine radiosonde launches occur one hour before the official observation times of 0000
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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
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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
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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
431:. A list of U.S. operated land based launch sites can be found in Appendix C, U.S. Land-based Rawinsonde Stations of the Federal Meteorological Handbook #3, titled Rawinsonde and Pibal Observations, dated May 1997. 270:
Diamond was given the Washington Academy of Sciences Engineering Award in 1940 and the IRE Fellow Award (which was later renamed the Harry Diamond Memorial Award) in 1943 for his contributions to radio-meteorology.
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launches radiosondes twice daily from 92 stations, 69 in the conterminous United States, 13 in Alaska, nine in the Pacific, and one in Puerto Rico. It also supports the operation of 10 radiosonde sites in the
1609: 1118: 118:("radar wind -sonde"). 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 1639: 975:"The Invention and Development of the Radiosonde, with a Catalog of Upper-Atmospheric Telemetering Probes in the National Museum of American History, Smithsonian Institution" 259:, who had previously worked on radio navigation and invented a blind landing system for airplanes. The organization led by Diamond eventually (in 1992) became a part of the 1798: 369:, 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 35:
sonde, approx 220 Ă— 80 Ă—75 mm (8.7 Ă— 3.1 Ă— 3 in) (with grounding station in the background, used to perform a 'ground check' and also recondition the humidity sensor)
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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
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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
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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
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Raw upper air data is routinely processed by supercomputers running numerical models. Forecasters often view the data in a graphical format, plotted on
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Gillmor, Stewart (December 26, 1989). "Seventy Years of Radio Science, Technology, Standards, and Measurement at the National Bureau of Standards".
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Ding, Tong; Awange, Joseph L.; Scherllin-Pirscher, Barbara; Kuhn, Michael; Anyah, Richard; Zerihun, Ayalsew; Bui, Luyen K. (16 September 2022).
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services during the 1930s and their increasing need for data motivated many nations to begin regular radiosonde observation programs
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or 1680 MHz. A radiosonde whose position is tracked as it ascends to give wind speed and direction information is called a
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ITU Radio Regulations, CHAPTER II – Frequencies, ARTICLE 5 Frequency allocations, Section IV – Table of Frequency Allocations
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and 1200 UTC to center the observation times during the roughly two-hour ascent. Radiosonde observations are important for
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However, military usage, in bands where there is civil usage, will be in accordance with the ITU Radio Regulations.
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suffered a loss of control after striking a radiosonde in flight resulting in the death of all 45 people on board.
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and transmits them by radio to a ground receiver. Modern radiosondes measure or calculate the following variables:
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RS41 radiosondes four times daily (an hour before 00, 06, 12, and 18 UTC) from 6 launch sites (south to north):
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The first flights of aerological instruments were done in the second half of the 19th century with kites and
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Bell, Tyler M.; Greene, Brian R.; Klein, Petra M.; Carney, Matthew; Chilson, Phillip B. (2020-07-16).
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ITU Radio Regulations, Section IV. Radio Stations and Systems – Article 1.109, definition:
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ITU Radio Regulations, Section IV. Radio Stations and Systems – Article 1.50, definition:
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primary allocation: is indicated by writing in capital letters (see example below)
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to develop an official radiosonde for the Navy to use. The NBS gave the project to
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DuBois, Multhauf and Ziegler, "The Invention and Development of the Radiosonde",
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was announced in 1902 at the French Academy of Sciences. Other researchers, like
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exclusive or shared utilization: is within the responsibility of administrations
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U.S. Bureau of Standards personnel launch radiosonde near Washington, DC in 1936
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Did You Know? We’re testing new weather balloons: from Cornwall to Antarctica!
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Clarke, E.T. (September 1941). "The radiosonde: The stratosphere laboratory".
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used for meteorological, including hydrological, observations and exploration.
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meteorological aids service / meteorological aids radiocommunication service
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Vernoff, S. "Radio-Transmission of Cosmic Ray Data from the Stratosphere",
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McGrath, Ray; Semmler, Tido; Sweeney, Conor; Wang, Shiyu (15 Jul 2006).
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Radiosonde Observations and Their Use in SPARC-Related Investigations.
1020: 2016: 1981: 1976: 1971: 828: 491: 428: 385: 354: 119: 96: 44: 381:. The weight of a radiosonde is typically 250 g (8.8 oz). 2186: 587:, kite or parachute, and which transmits meteorological data. Each 580: 514:
regions in the stratosphere. This issue may in future be solved by
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A Century of Excellence in Measurements, Standards, and Technology
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The allocation of radio frequencies is provided according to
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Satellite emergency position-indicating radiobeacon station
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WMO spreadsheet of all Upper Air stations around the world
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data, and hundreds are launched all over the world daily.
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DuBois, John; Multhauf, Robert; Ziegler, Charles (2002).
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Modern radiosondes showing progress of miniaturisation
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might be primary, secondary, exclusive, and shared.
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US sailors launching a radiosonde during World War 2
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instrument carried into the atmosphere usually by a
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secondary allocation: is indicated by small letters
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National Oceanic and Atmospheric Administration 477: 446:, (lat,lon)=(50.218, -5.327), SW tip of England; 2199: 1157:"1943-radiosonde-fatality.JPG (758x1280 pixels)" 782: 595:in which it operates permanently or temporarily. 146:Meteograph used by the US Weather Bureau in 1898 1554:Upper air data for the world - past and present 825:National Oceanic and Atmospheric Administration 502:profile of temperature and moisture as well as 640: 545:meteorological aids radiocommunication service 391: 1939: 1625: 941:Smithsonian Studies in History and Technology 679:EARTH EXPLORATION-SATELLITE (Earth-to-space) 608:of the ITU Radio Regulations (edition 2012). 2228:Meteorological instrumentation and equipment 1956:meteorological equipment and instrumentation 1209:Journal of Geophysical Research: Atmospheres 1198: 1196: 1194: 1192: 1190: 1001:Eos, Transactions American Geophysical Union 530: 2238:Science and technology in the Soviet Union 1946: 1932: 1803:Standard frequency and time signal station 1632: 1618: 186:Observatoire de MĂ©tĂ©orologie Dynamique de 122:. Radiosondes are an essential source of 1459: 1418: 1236: 1187: 835: 681:METEOROLOGICAL-SATELLITE (Earth-to-space) 1575:Radiosonde Sounding System at webmet.com 641: 305:. The sondes were tracked for two days. 157: 149: 141: 133: 103:concentration are known as ozonesondes. 26: 18: 1297: 1295: 998: 599: 211:In 1924, Colonel William Blaire in the 2200: 1099:nistdigitalarchives.contentdm.oclc.org 1036: 935: 933: 807: 805: 662:401-402 MHz       2253:International Telecommunication Union 1927: 1613: 1566:Tephigrams and Skew-T log P diagrams. 1062: 1060: 1032: 1030: 876:DĂ©couvrir : Mesurer l’atmosphère 866: 864: 537:International Telecommunication Union 301:, each dropped a radiosonde into the 1333:"Federal Meteorological Handbook #3" 1292: 1066: 968: 966: 964: 962: 733:Global horizontal sounding technique 251:In 1936, the U.S. Navy assigned the 1645:          1605:Photo - Radiosonde, Transistor Type 1369:Protecting our observing capability 930: 849:. Encyclopædia Britannica Inc. 2014 802: 783:Karin L. Gleason (March 20, 2008). 13: 1570:Radiosonde Museum of North America 1440:Atmospheric Measurement Techniques 1314:U.S. Land-based Rawinsode Stations 1057: 1027: 897: 861: 462:, (55.02, -1.88), NE England; and 14: 2269: 1547: 1039:Journal of the Franklin Institute 959: 909:La mĂ©tĂ©o de A Ă  Z > DĂ©finition 685:Mobile except aeronautical mobile 677:SPACE OPERATION (space-to-Earth) 524:World Meteorological Organisation 1907: 1898: 1897: 1640: 1252: 349:lifts the device up through the 1839:Instrument landing system (ILS) 1787:Radio direction-finding station 1649:and systems in accordance with 1532: 1520: 1508: 1490: 1476: 1427: 1386: 1374: 1362: 1350: 1325: 1307: 1280: 1265: 1167: 1149: 1140: 1111: 1087: 980:. Smithsonian Institution Press 450:(50.89, 0.318), near SE coast; 2248:Radio stations and systems ITU 1771:Radionavigation mobile station 1739:On-board communication station 1687:High altitude platform station 1277:. Retrieved February 19, 2017. 992: 946: 847:Encyclopædia Britannica online 776: 478:Uses of upper air observations 253:U.S. Bureau of Standards (NBS) 138:Kites used to fly a meteograph 87:readings at high altitude and 16:Meteorological instrumentation 1: 1600:Photo - Early Type Radiosonde 1381:Synoptic and climate stations 1051:10.1016/S0016-0032(41)90950-X 817:Upper-air observation program 769: 571:A radiosonde is an automatic 416:, and atmospheric research. 261:U.S. Army Research Laboratory 106:Radiosondes may operate at a 2208:Telecommunications equipment 1819:Ship's emergency transmitter 1779:Radiolocation mobile station 1775:Radionavigation land station 1564:Interpreting radiosonde data 647: 328: 7: 1272:WMO Global Observing System 821:US National Weather Service 701: 593:radiocommunication service 591:shall be classified by the 577:meteorological aids service 541:meteorological aids service 392:Routine radiosonde launches 341:balloon filled with either 10: 2276: 2213:Atmospheric thermodynamics 1815:Experimental radio station 1783:Radiolocation land station 1767:Radiodetermination station 1751:Aeronautical earth station 1335:. Ofcm.gov. Archived from 723:Atmospheric thermodynamics 563:Furthermore, according to 559:radiocommunication service 510:except perhaps locally in 506:of vertical wind profile. 129: 1962: 1893: 1719:Land mobile earth station 1657: 1585:Sergei Nikolaevich Vernov 1383:Retrieved 1 January 2023. 1371:Retrieved 1 January 2023. 1359:Retrieved 1 January 2023. 1304:Retrieved 1 January 2023. 1289:Retrieved 1 January 2023. 1073:. CRC Press. p. 42. 661: 99:). Radiosondes measuring 1887:Emergency locator beacon 1502:South China Morning Post 1461:10.5194/amt-13-3855-2020 1184:Retrieved on 2008-05-25. 713:Aerography (meteorology) 531:International regulation 424:National Weather Service 281:In 1985, as part of the 2037:Ice accretion indicator 1811:Radio astronomy station 759:Water-activated battery 182:LĂ©on Teisserenc de Bort 2077:Present weather sensor 1759:Aircraft earth station 1679:Survival craft station 1319:March 3, 2016, at the 1275:Upper-air observations 643:Allocation to services 597: 579:usually carried on an 484:thermodynamic diagrams 375:radio direction finder 246:Earth's magnetic field 163: 155: 147: 139: 53:atmospheric parameters 51:that measures various 36: 24: 2223:Measuring instruments 1651:ITU Radio Regulations 1180:June 7, 2007, at the 569: 553:ITU Radio Regulations 488:Skew-T log-P diagrams 458:in Northern Ireland; 161: 153: 145: 137: 89:geographical position 43:is a battery-powered 30: 22: 2258:Atmospheric sounding 2002:Dark adaptor goggles 1879:Multi-satellite link 1835:Radar beacon (racon) 1791:Radio beacon station 1763:Broadcasting station 1747:Aeronautical station 1695:Mobile earth station 1229:10.1029/2022JD036648 1067:Lide, David (2001). 632:frequency allocation 600:Frequency allocation 547:) is – according to 466:, (60.139, -1.183), 414:watches and warnings 323:Aeroflot Flight 1661 1727:Coast earth station 1715:Land mobile station 1667:Terrestrial station 1452:2020AMT....13.3855B 1411:2006JCli...19.3430M 1221:2022JGRD..12736648D 1163:on 8 February 2013. 1013:1989EOSTr..70.1571G 664:METEOROLOGICAL AIDS 407:weather forecasting 303:atmosphere of Venus 276:weather forecasting 206:William Henry Dines 2233:Russian inventions 2047:Lightning detector 1735:Ship earth station 1711:Base earth station 1703:Land earth station 1504:. 31 October 2021. 1420:10.1175/JCLI3804.1 1399:Journal of Climate 1238:20.500.11937/91903 555:(RR) – defined as 164: 156: 148: 140: 37: 25: 2243:Soviet inventions 2218:French inventions 2195: 2194: 2137:Thermo-hygrograph 2127:Sunshine recorder 1992:Ceiling projector 1921: 1920: 1871:Satellite network 1405:(14): 3430–3442. 1287:Weather Balloons! 1080:978-0-8493-1247-2 1021:10.1029/89EO00403 905:"Bureau (Robert)" 718:Atmospheric model 699: 698: 589:radio transmitter 573:radio transmitter 535:According to the 213:U.S. Signal Corps 184:organized at the 69:relative humidity 2265: 2177:Whole sky camera 2122:Stevenson screen 2027:Heat flux sensor 1948: 1941: 1934: 1925: 1924: 1911: 1901: 1900: 1867:Satellite system 1755:Aircraft station 1662: 1644: 1634: 1627: 1620: 1611: 1610: 1541: 1536: 1530: 1524: 1518: 1512: 1506: 1505: 1494: 1488: 1487: 1480: 1474: 1473: 1463: 1446:(7): 3855–3872. 1431: 1425: 1424: 1422: 1390: 1384: 1378: 1372: 1366: 1360: 1354: 1348: 1347: 1345: 1344: 1329: 1323: 1311: 1305: 1299: 1290: 1284: 1278: 1269: 1263: 1256: 1250: 1240: 1200: 1185: 1173:Dian J. 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Index



GPS
telemetry
weather balloon
atmospheric parameters
altitude
pressure
temperature
relative humidity
wind
wind speed
wind direction
cosmic ray
geographical position
latitude
longitude
ozone
radio frequency
MHz
dropsonde
meteorological




meteographs
Gustave Hermite
Georges Besançon
LĂ©on Teisserenc de Bort

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