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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.
1265: 364:. 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 170: 154: 1653: 1910: 1920: 538:
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.
39: 274:. 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. 181:, 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. 407:
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
442:. 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. 281:
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
1620: 1129: 129:("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 1650: 986:"The Invention and Development of the Radiosonde, with a Catalog of Upper-Atmospheric Telemetering Probes in the National Museum of American History, Smithsonian Institution" 270:, 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 1809: 380:, 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 46:
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
1949: 1391: 271: 238:. Bureau coined the name "radiosonde" and flew the first instrument on January 7, 1929. Developed independently a year later, 2218: 1605: 1550:
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.
1031: 2027: 1992: 1987: 1982: 839: 502: 439: 396: 365: 130: 107: 55: 392:. The weight of a radiosonde is typically 250 g (8.8 oz). 2197: 598:, kite or parachute, and which transmits meteorological data. Each 591: 525:
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 488: 457:, (lat,lon)=(50.218, -5.327), SW tip of England; 2210: 1168:"1943-radiosonde-fatality.JPG (758x1280 pixels)" 793: 606:in which it operates permanently or temporarily. 157:Meteograph used by the US Weather Bureau in 1898 1565:Upper air data for the world - past and present 836:National Oceanic and Atmospheric Administration 513:profile of temperature and moisture as well as 651: 556:meteorological aids radiocommunication service 402: 1950: 1636: 952:Smithsonian Studies in History and Technology 690:EARTH EXPLORATION-SATELLITE (Earth-to-space) 619:of the ITU Radio Regulations (edition 2012). 2239:Meteorological instrumentation and equipment 1967:meteorological equipment and instrumentation 1220:Journal of Geophysical Research: Atmospheres 1209: 1207: 1205: 1203: 1201: 1012:Eos, Transactions American Geophysical Union 541: 2249:Science and technology in the Soviet Union 1957: 1943: 1814:Standard frequency and time signal station 1643: 1629: 197:Observatoire de MĂ©tĂ©orologie Dynamique de 133:. Radiosondes are an essential source of 1470: 1429: 1247: 1198: 846: 692:METEOROLOGICAL-SATELLITE (Earth-to-space) 1586:Radiosonde Sounding System at webmet.com 652: 316:. The sondes were tracked for two days. 168: 160: 152: 144: 114:concentration are known as ozonesondes. 37: 29: 1308: 1306: 1009: 610: 222:In 1924, Colonel William Blaire in the 14: 2211: 1110:nistdigitalarchives.contentdm.oclc.org 1047: 946: 944: 818: 816: 673:401-402 MHz       2264:International Telecommunication Union 1938: 1624: 1577:Tephigrams and Skew-T log P diagrams. 1073: 1071: 1043: 1041: 887:DĂ©couvrir : Mesurer l’atmosphère 877: 875: 548:International Telecommunication Union 312:, each dropped a radiosonde into the 1344:"Federal Meteorological Handbook #3" 1303: 1077: 979: 977: 975: 973: 744:Global horizontal sounding technique 262:In 1936, the U.S. Navy assigned the 1656:          1616:Photo - Radiosonde, Transistor Type 1380:Protecting our observing capability 941: 860:. Encyclopædia Britannica Inc. 2014 813: 794:Karin L. Gleason (March 20, 2008). 24: 1581:Radiosonde Museum of North America 1451:Atmospheric Measurement Techniques 1325:U.S. Land-based Rawinsode Stations 1068: 1038: 908: 872: 473:, (55.02, -1.88), NE England; and 25: 2280: 1558: 1050:Journal of the Franklin Institute 970: 920:La mĂ©tĂ©o de A Ă  Z > DĂ©finition 696:Mobile except aeronautical mobile 688:SPACE OPERATION (space-to-Earth) 535:World Meteorological Organisation 1918: 1909: 1908: 1651: 1263: 360:lifts the device up through the 1850:Instrument landing system (ILS) 1798:Radio direction-finding station 1660:and systems in accordance with 1543: 1531: 1519: 1501: 1487: 1438: 1397: 1385: 1373: 1361: 1336: 1318: 1291: 1276: 1178: 1160: 1151: 1122: 1098: 991:. Smithsonian Institution Press 461:(50.89, 0.318), near SE coast; 2259:Radio stations and systems ITU 1782:Radionavigation mobile station 1750:On-board communication station 1698:High altitude platform station 1288:. Retrieved February 19, 2017. 1003: 957: 858:Encyclopædia Britannica online 787: 489:Uses of upper air observations 264:U.S. Bureau of Standards (NBS) 149:Kites used to fly a meteograph 98:readings at high altitude and 27:Meteorological instrumentation 13: 1: 1611:Photo - Early Type Radiosonde 1392:Synoptic and climate stations 1062:10.1016/S0016-0032(41)90950-X 828:Upper-air observation program 780: 582:A radiosonde is an automatic 427:, and atmospheric research. 272:U.S. Army Research Laboratory 117:Radiosondes may operate at a 2219:Telecommunications equipment 1830:Ship's emergency transmitter 1790:Radiolocation mobile station 1786:Radionavigation land station 1575:Interpreting radiosonde data 658: 339: 7: 1283:WMO Global Observing System 832:US National Weather Service 712: 604:radiocommunication service 602:shall be classified by the 588:meteorological aids service 552:meteorological aids service 403:Routine radiosonde launches 352:balloon filled with either 10: 2285: 2224:Atmospheric thermodynamics 1826:Experimental radio station 1794:Radiolocation land station 1778:Radiodetermination station 1762:Aeronautical earth station 1346:. Ofcm.gov. Archived from 734:Atmospheric thermodynamics 574:Furthermore, according to 570:radiocommunication service 521:except perhaps locally in 517:of vertical wind profile. 140: 1973: 1904: 1730:Land mobile earth station 1668: 1596:Sergei Nikolaevich Vernov 1394:Retrieved 1 January 2023. 1382:Retrieved 1 January 2023. 1370:Retrieved 1 January 2023. 1315:Retrieved 1 January 2023. 1300:Retrieved 1 January 2023. 1084:. CRC Press. p. 42. 672: 110:). Radiosondes measuring 1898:Emergency locator beacon 1513:South China Morning Post 1472:10.5194/amt-13-3855-2020 1195:Retrieved on 2008-05-25. 724:Aerography (meteorology) 542:International regulation 435:National Weather Service 292:In 1985, as part of the 2048:Ice accretion indicator 1822:Radio astronomy station 770:Water-activated battery 193:LĂ©on Teisserenc de Bort 2088:Present weather sensor 1770:Aircraft earth station 1690:Survival craft station 1330:March 3, 2016, at the 1286:Upper-air observations 654:Allocation to services 608: 590:usually carried on an 495:thermodynamic diagrams 386:radio direction finder 257:Earth's magnetic field 174: 166: 158: 150: 64:atmospheric parameters 62:that measures various 47: 35: 2234:Measuring instruments 1662:ITU Radio Regulations 1191:June 7, 2007, at the 580: 564:ITU Radio Regulations 499:Skew-T log-P diagrams 469:in Northern Ireland; 172: 164: 156: 148: 100:geographical position 54:is a battery-powered 41: 33: 2269:Atmospheric sounding 2013:Dark adaptor goggles 1890:Multi-satellite link 1846:Radar beacon (racon) 1802:Radio beacon station 1774:Broadcasting station 1758:Aeronautical station 1706:Mobile earth station 1240:10.1029/2022JD036648 1078:Lide, David (2001). 643:frequency allocation 611:Frequency allocation 558:) is – according to 477:, (60.139, -1.183), 425:watches and warnings 334:Aeroflot Flight 1661 1738:Coast earth station 1726:Land mobile station 1678:Terrestrial station 1463:2020AMT....13.3855B 1422:2006JCli...19.3430M 1232:2022JGRD..12736648D 1174:on 8 February 2013. 1024:1989EOSTr..70.1571G 675:METEOROLOGICAL AIDS 418:weather forecasting 314:atmosphere of Venus 287:weather forecasting 217:William Henry Dines 2244:Russian inventions 2058:Lightning detector 1746:Ship earth station 1722:Base earth station 1714:Land earth station 1515:. 31 October 2021. 1431:10.1175/JCLI3804.1 1410:Journal of Climate 1249:20.500.11937/91903 566:(RR) – defined as 175: 167: 159: 151: 48: 36: 2254:Soviet inventions 2229:French inventions 2206: 2205: 2148:Thermo-hygrograph 2138:Sunshine recorder 2003:Ceiling projector 1932: 1931: 1882:Satellite network 1416:(14): 3430–3442. 1298:Weather Balloons! 1091:978-0-8493-1247-2 1032:10.1029/89EO00403 916:"Bureau (Robert)" 729:Atmospheric model 710: 709: 600:radio transmitter 584:radio transmitter 546:According to the 224:U.S. Signal Corps 195:organized at the 80:relative humidity 16:(Redirected from 2276: 2188:Whole sky camera 2133:Stevenson screen 2038:Heat flux sensor 1959: 1952: 1945: 1936: 1935: 1922: 1912: 1911: 1878:Satellite system 1766:Aircraft station 1673: 1655: 1645: 1638: 1631: 1622: 1621: 1552: 1547: 1541: 1535: 1529: 1523: 1517: 1516: 1505: 1499: 1498: 1491: 1485: 1484: 1474: 1457:(7): 3855–3872. 1442: 1436: 1435: 1433: 1401: 1395: 1389: 1383: 1377: 1371: 1365: 1359: 1358: 1356: 1355: 1340: 1334: 1322: 1316: 1310: 1301: 1295: 1289: 1280: 1274: 1267: 1261: 1251: 1211: 1196: 1184:Dian J. 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Index

Rawinsonde


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

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