The ECMWF reanalysis project is a meteorological reanalysis project carried out by the European Centre for Medium-Range Weather Forecasts (ECMWF). The first reanalysis product, ERA-15 , generated reanalyses for approximately 15 years, from December 1978 to February 1994. The second product, ERA-40 (originally intended as a 40-year reanalysis) begins in 1957 (the International Geophysical Year ) and covers 45 years to 2002. As a precursor to a revised extended reanalysis product to replace ERA-40, ECMWF released ERA-Interim , which covers the period from 1979 to 2019. A new reanalysis product ERA5 has more recently been released by ECMWF as part of Copernicus Climate Change Services. This product has higher spatial resolution (31 km) and covers the period from 1979 to present. Extension up to 1940 became available in 2023.
36-446: In addition to reanalysing all the old data using a consistent system, the reanalyses also make use of much archived data that was not available to the original analyses. This allows for the correction of many historical hand-drawn maps where the estimation of features was common in areas of data sparsity. The ability is also present to create new maps of atmosphere levels that were not commonly used until more recent times. Many sources of
72-683: 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 . 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 understanding weather conditions and climate trends and providing weather and climate information for
108-492: 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"). 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
144-501: A blind landing system for airplanes. The organization led by Diamond eventually (in 1992) became a part of the U.S. Army Research Laboratory . 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
180-516: 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
216-521: 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. 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. This became an important technique in
252-425: A small parachute 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 Clark Air Base , Philippines, reached an altitude of 155,092 ft (47,272 m). The modern radiosonde communicates via radio with
288-754: Is illegal in France). A man on the terrorism watch list of the French police, killed his mother and sister with a knife in Trappes on August 23, 2018. Amaq News Agency claimed responsibility on behalf of the Islamic State. However, French interior minister Gérard Collomb stated he was a man with mental health issues, rather than someone inspired by the organisation. There are 36 municipal preschools and primary schools in Trappes. The community has three junior high schools: Senior high schools/sixth form colleges: Trappes
324-550: Is a banlieue located in the western outer suburbs of Paris , 26.7 km (16.6 mi) from the centre of Paris , part of the new town of Saint-Quentin-en-Yvelines . Trappes is served by Trappes station on the Transilien La Défense and Transilien Paris-Montparnasse suburban rail lines. The suburb is known for gang violence and poverty . It also has Islamists among its large Muslim population, with 70 local people suspected of having left France to fight for
360-659: Is a stub . You can help Misplaced Pages by expanding it . Radiosondes A radiosonde is a battery-powered telemetry instrument carried into the atmosphere usually by a weather balloon that measures various atmospheric parameters and transmits them by radio to a ground receiver. Modern radiosondes measure or calculate the following variables: altitude , pressure , temperature , relative humidity , wind (both wind speed and wind direction ), cosmic ray readings at high altitude and geographical position ( latitude / longitude ). Radiosondes measuring ozone concentration are known as ozonesondes. Radiosondes may operate at
396-537: Is with-in the responsibility of the appropriate national administration. The allocation might be primary, secondary, exclusive, and shared. However, military usage, in bands where there is civil usage, will be in accordance with the ITU Radio Regulations. Trappes Trappes ( French: [tʁap] ) is a commune in the Yvelines department , Île-de-France region , Northern France . It
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#1732858276406432-612: Is – according to Article 1.50 of the ITU Radio Regulations (RR) – defined as "A radiocommunication service used for meteorological, including hydrological, observations and exploration. Furthermore, according to article 1.109 of the ITU RR: A radiosonde is an automatic radio transmitter in the meteorological aids service usually carried on an aircraft , free balloon , kite or parachute, and which transmits meteorological data. Each radio transmitter shall be classified by
468-466: The Islamic State , according to several sources. According to the French government, 67 people from Trappes have joined the Islamic State, and others have carried out attacks inside France. In July 2013, Trappes police station was attacked by a mob of French Muslims in response to the arrest of a man who had assaulted a police officer during an identity check on his entirely veiled wife (face covering
504-722: 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. Although hundreds of radiosondes are launched worldwide each day year-round, fatalities attributed to radiosondes are rare. The first known example
540-602: The World Meteorological Organisation 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 Africa have experienced severe (57%) and moderate (25%) radiosonde data gap. This dire situation has prompted call for urgent need to fill
576-500: 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). After bursting,
612-412: The radiocommunication service in which it operates permanently or temporarily. The allocation of radio frequencies is provided according to Article 5 of the ITU Radio Regulations (edition 2012). 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
648-455: 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
684-521: The SE corner of Lough Neagh in Northern Ireland; Albemarle , (55.02, -1.88), NE England; and Lerwick , (60.139, -1.183), Shetland , Scotland . Raw upper air data is routinely processed by supercomputers running 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
720-570: The atmospheric state. The ECMWF re-analysis products are accessible from the Climate Change Services homepage. The data can be downloaded for research use from ECMWF's homepage (see external links) and the National Center for Atmospheric Research data archives. Both require registration. A Python web API can be used to download a subset of parameters for a selected region and time period. This article about atmospheric science
756-532: 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. According to the International Telecommunication Union , a meteorological aids service (also: meteorological aids radiocommunication service )
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#1732858276406792-494: 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 . In 1936, the U.S. Navy assigned the U.S. Bureau of Standards (NBS) to develop an official radiosonde for the Navy to use. The NBS gave the project to Harry Diamond , who had previously worked on radio navigation and invented
828-501: 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
864-467: The link to the ground. Gustave Hermite and Georges Besançon , from France, were the first in 1892 to use a balloon to fly the meteograph. In 1898, Léon Teisserenc de Bort organized at the Observatoire de Météorologie Dynamique de 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
900-516: The meteorological observations were used, including radiosondes , balloons , aircraft , buoyes , satellites , scatterometers . This data was run through the ECMWF computer model at a 125 km resolution. As the ECMWF's computer model is one of the more highly regarded in the field of forecasting, many scientists take its reanalysis to have similar merit. The data is stored in GRIB format. The reanalysis
936-559: The observation times during the roughly two-hour ascent. Radiosonde observations are important for weather forecasting , severe weather watches and warnings , and atmospheric research. The United States National Weather Service 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
972-775: 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 of the Federal Meteorological Handbook #3, titled Rawinsonde and Pibal Observations, dated May 1997. The UK launches Vaisala RS41 radiosondes four times daily (an hour before 00, 06, 12, and 18 UTC) from 6 launch sites (south to north): Camborne , (lat,lon)=(50.218, -5.327), SW tip of England; Herstmonceux (50.89, 0.318), near SE coast; Watnall , (53.005, -1.25), central England; Castor Bay, (54.50, -6.34), near
1008-502: 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. 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
1044-421: The stratosphere. This issue may in future be solved by weather drones , which have precise control over their location and can compensate for drift. 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
1080-451: 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 [ fr ] . Bureau coined the name "radiosonde" and flew the first instrument on January 7, 1929. Developed independently a year later, Pavel Molchanov flew a radiosonde on January 30, 1930. Molchanov's design became
1116-413: The time due to the use of electric sensors. 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 collect weather data in remote and inhospitable locations. By 1940,
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1152-431: The welfare of societies. Reliable and timely information underpin society’s preparedness to extreme weather conditions and to changing climate patterns. 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 UTC and 1200 UTC to center
1188-432: The world daily. 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 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
1224-405: Was done in an effort to improve the accuracy of historical weather maps and aid in a more detailed analysis of various weather systems through a period that was severely lacking in computerized data. With the data from reanalyses such as this, many of the more modern computerized tools for analyzing storm systems can be utilized, at least in part, because of this access to a computerized simulation of
1260-692: Was officially adopted by the U.S. Weather Bureau. 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. The expansion of economically important government weather forecasting services during the 1930s and their increasing need for data motivated many nations to begin regular radiosonde observation programs In 1985, as part of
1296-467: 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 Antonov 24 operating Aeroflot Flight 1661 suffered a loss of control after striking a radiosonde in flight resulting in the death of all 45 people on board. A rubber or latex balloon filled with either helium or hydrogen lifts the device up through
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