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Meteorology
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{{About|the study of weather|the science of measurement|Metrology|the study of meteors|Meteoritics}}{{about||other uses of the root word "meteor"|Meteor (disambiguation)|the work by Aristotle|Meteorology (Aristotle)}}{{Weather}}{{Atmospheric sciences}}Meteorology is a branch of the atmospheric sciences which includes atmospheric chemistry and atmospheric physics, with a major focus on weather forecasting. The study of meteorology dates back millennia, though significant progress in meteorology did not occur until the 18th century. The 19th century saw modest progress in the field after weather observation networks were formed across broad regions. Prior attempts at prediction of weather depended on historical data. It wasn't until after the elucidation of the laws of physics and, more particularly, the development of the computer, allowing for the automated solution of a great many equations that model the weather, in the latter half of the 20th century that significant breakthroughs in weather forecasting were achieved.Meteorological phenomena are observable weather events that are explained by the science of meteorology. Meteorological phenomena are described and quantified by the variables of Earth's atmosphere: temperature, air pressure, water vapour, mass flow, and the variations and interactions of those variables, and how they change over time. Different spatial scales are used to describe and predict weather on local, regional, and global levels.
Meteorology, climatology, atmospheric physics, and atmospheric chemistry are sub-disciplines of the atmospheric sciences. Meteorology and hydrology compose the interdisciplinary field of hydrometeorology. The interactions between Earth's atmosphere and its oceans are part of a coupled ocean-atmosphere system. Meteorology has application in many diverse fields such as the military, energy production, transport, agriculture, and construction.The word "(wikt:meteorology|meteorology)" is from Greek (wikt:μετέωρος|μετέωρος) metéōros "meteor" and (wikt:-λογία|-λογία) -logia "(wikt:-logy|-(o)logy)", i.e. "the study of things in the air".

History

File:AlpineRainbow.jpg|thumb|left|Parhelion (sundog) in SavoieSavoieThe ability to predict rains and floods based on annual cycles was evidently used by humans at least from the time of agricultural settlement if not earlier. Early approaches to predicting weather were based on astrology and were practiced by priests. Cuneiform inscriptions on Babylonian tablets included associations between thunder and rain. The Chaldeans differentiated the 22° and 46° halos.JOURNAL, Hellmann, G., 1908-10-01, The dawn of meteorology,weblink Quarterly Journal of the Royal Meteorological Society, en, 34, 148, 221–232, 10.1002/qj.49703414802, 1477-870X, 1908QJRMS..34..221H, Ancient Indian Upanishads contain mentions of clouds and seasons.WEB, NS, nsimd@ymail.com,weblink History of Meteorology in India, Imd.gov.in, 2012-03-25, yes,weblink" title="web.archive.org/web/20120330125208weblink">weblink 2012-03-30, The Samaveda mentions sacrifices to be performed when certain phenomena were noticed. Varāhamihira's classical work Brihatsamhita, written about 500 AD, provides evidence of weather observation.In 350 BC, Aristotle wrote Meteorology.WEB,weblink meteorology: Introduction, 16 June 2015, Aristotle is considered the founder of meteorology.WEB,weblink 94.05.01: Meteorology, 16 June 2015, One of the most impressive achievements described in the Meteorology is the description of what is now known as the hydrologic cycle.BOOK, Aristotle, Meteorology,weblink 2004, eBooks@Adelaide, The University of Adelaide Library, University of Adelaide, South Australia 5005, Translated by E.W. Webster, 350 BCE, yes,weblink" title="web.archive.org/web/20070217110549weblink">weblink 2007-02-17, The book De Mundo (composed before 250 BC or between 350 and 200 BC) notedBOOK,weblink De Mundo, 1914, Aristotle; Forster, E. S. (Edward Seymour), 1879-1950; Dobson, J. F. (John Frederic), 1875-1947, Chapter 4,
If the flashing body is set on fire and rushes violently to the Earth it is called a thunderbolt; if it is only half of fire, but violent also and massive, it is called a meteor; if it is entirely free from fire, it is called a smoking bolt. They are all called 'swooping bolts' because they swoop down upon the Earth. Lightning is sometimes smoky, and is then called 'smoldering lightning"; sometimes it darts quickly along, and is then said to be vivid. At other times, it travels in crooked lines, and is called forked lightning. When it swoops down upon some object it is called 'swooping lightning'.
The Greek scientist Theophrastus compiled a book on weather forecasting, called the Book of Signs. The work of Theophrastus remained a dominant influence in the study of weather and in weather forecasting for nearly 2,000 years.WEB,weblink Weather, 16 June 2015, In 25 AD, Pomponius Mela, a geographer for the Roman Empire, formalized the climatic zone system.WEB,weblink Timeline of geography, paleontology, Paleorama.com, Following the path of Discovery, According to Toufic Fahd, around the 9th century, Al-Dinawari wrote the Kitab al-Nabat (Book of Plants), in which he deals with the application of meteorology to agriculture during the Muslim Agricultural Revolution. He describes the meteorological character of the sky, the planets and constellations, the sun and moon, the lunar phases indicating seasons and rain, the anwa (heavenly bodies of rain), and atmospheric phenomena such as winds, thunder, lightning, snow, floods, valleys, rivers, lakes.JOURNAL, Fahd, Toufic, Botany and agriculture, 815, BOOK, Morelon, Régis, Rashed, Roshdi, 1996, Encyclopedia of the History of Arabic Science, 3, Routledge, 0-415-12410-7, {{Verify source|date=September 2010}}Early attempts at predicting weather were often related to prophesy and divining and sometimes based on astrological ideas. Admiral FitzRoy tried to separate scientific approaches from prophetic ones.JOURNAL, Anderson, Katharine, 1999, The weather prophets: science and reputation in Victorian meteorology, History of Science, 37, 179–215, 1999HisSc..37..179A,

Research of visual atmospheric phenomena

File:Baker beach at twilight 41.jpg|Twilight at thumb{{See also|Rainbow|Twilight}}Ptolemy wrote on the atmospheric refraction of light in the context of astronomical observations.Smith AM, 1996. "Ptolemy's Theory of Visual Perception: An English Translation of the Optics," pp. 46. Transactions of the American Philosophical Society vol. 86, part 2. In 1021, Alhazen showed that atmospheric refraction is also responsible for twilight; he estimated that twilight begins when the sun is 19 degrees below the horizon, and also used a geometric determination based on this to estimate the maximum possible height of the Earth's atmosphere as 52,000 passim (about 49 miles, or 79 km).Frisinger H (1973), "Aristotle's Legacy in Meteorology." Bulletin of the American Meteorological Society volume 3 issue 3, pp. 198–204. Link.St. Albert the Great was the first to propose that each drop of falling rain had the form of a small sphere, and that this form meant that the rainbow was produced by light interacting with each raindrop.WEB,weblink Ancient and pre-Renaissance Contributors to Meteorology, 16 June 2015, Roger Bacon was the first to calculate the angular size of the rainbow. He stated that a rainbow summit can not appear higher than 42 degrees above the horizon.The rainbow bridge: rainbows in art, myth, and science, p.156, Raymond L. Lee, Alistair B. Fraser In the late 13th century and early 14th century, Kamāl al-DÄ«n al-FārisÄ« and Theodoric of Freiberg were the first to give the correct explanations for the primary rainbow phenomenon. Theoderic went further and also explained the secondary rainbow.Topdemir, Hüseyin Gazi (2007), Kamal Al-din Al-Farisi's explanation of the rainbow In 1716, Edmund Halley suggested that aurorae are caused by "magnetic effluvia" moving along the Earth's magnetic field lines.

Instruments and classification scales

{{See also|Beaufort Scale|Celsius|Fahrenheit}}(File:Wea00920.jpg|thumb|A hemispherical cup anemometer)In 1441, King Sejong's son, Prince Munjong, invented the first standardized rain gauge.BOOK,weblink's+son,+Prince+Munjong,+invented+the+first+standardized+rain+gauge&hl=en&sa=X&ved=0ahUKEwj10ffs7vrUAhUF1GMKHdThDUQQ6AEIJDAA#v=onepage&q=In%201441,%20King%20Sejong's%20son,%20Prince%20Munjong,%20invented%20the%20first%20standardized%20rain%20gauge&f=false, Earth Science' 2005 Ed., Rex Bookstore, Inc., 9789712339387, en, These were sent throughout the Joseon Dynasty of Korea as an official tool to assess land taxes based upon a farmer's potential harvest. In 1450, Leone Battista Alberti developed a swinging-plate anemometer, and was known as the first anemometer.BOOK, Jacobson, Mark Z., Fundamentals of Atmospheric Modeling, paperback, 2nd, June 2005, Cambridge University Press, New York, 978-0-521-54865-6, 828, In 1607, Galileo Galilei constructed a thermoscope. In 1611, Johannes Kepler wrote the first scientific treatise on snow crystals: "Strena Seu de Nive Sexangula (A New Year's Gift of Hexagonal Snow)".WEB,weblink Early Snow Crystal Observations, 16 June 2015, In 1643, Evangelista Torricelli invented the mercury barometer. In 1662, Sir Christopher Wren invented the mechanical, self-emptying, tipping bucket rain gauge. In 1714, Gabriel Fahrenheit created a reliable scale for measuring temperature with a mercury-type thermometer.Grigull, U., Fahrenheit, a Pioneer of Exact Thermometry. Heat Transfer, 1966, The Proceedings of the 8th International Heat Transfer Conference, San Francisco, 1966, Vol. 1. In 1742, Anders Celsius, a Swedish astronomer, proposed the "centigrade" temperature scale, the predecessor of the current Celsius scale.Beckman, Olof,History of the Celsius temperature scale., translated, Anders Celsius (Elementa,84:4,2001); English In 1783, the first hair hygrometer was demonstrated by Horace-Bénédict de Saussure. In 1802–1803, Luke Howard wrote On the Modification of Clouds, in which he assigns cloud types Latin names.Thornes, John. E. (1999). John Constable's Skies. The University of Birmingham Press, pp. 189. {{ISBN|1-902459-02-4}}. In 1806, Francis Beaufort introduced his system for classifying wind speeds.Bill Giles O.B.E. (2009). Beaufort Scale. BBC. Retrieved on 2009-05-12. Near the end of the 19th century the first cloud atlases were published, including the International Cloud Atlas, which has remained in print ever since. The April 1960 launch of the first successful weather satellite, TIROS-1, marked the beginning of the age where weather information became available globally.

Atmospheric composition research

In 1648, Blaise Pascal rediscovered that atmospheric pressure decreases with height, and deduced that there is a vacuum above the atmosphere.Florin to Pascal, September 1647, Œuves completes de Pascal, 2:682. In 1738, Daniel Bernoulli published Hydrodynamics, initiating the Kinetic theory of gases and established the basic laws for the theory of gases.{{MacTutor Biography|id=Bernoulli_Daniel}} In 1761, Joseph Black discovered that ice absorbs heat without changing its temperature when melting. In 1772, Black's student Daniel Rutherford discovered nitrogen, which he called phlogisticated air, and together they developed the phlogiston theory.Biographical note at "Lectures and Papers of Professor Daniel Rutherford (1749–1819), and Diary of Mrs Harriet Rutherford". In 1777, Antoine Lavoisier discovered oxygen and developed an explanation for combustion."Sur la combustion en général" ("On Combustion in general," 1777) and "Considérations Générales sur la Nature des Acides" ("General Considerations on the Nature of Acids," 1778). In 1783, in Lavoisier's essay "Reflexions sur le phlogistique",Nicholas W. Best, "Lavoisier's 'Reflections on Phlogiston' I: Against Phlogiston Theory", Foundations of Chemistry, 2015, 17, 137-151. he deprecates the phlogiston theory and proposes a caloric theory.Nicholas W. Best, Lavoisier's 'Reflections on Phlogiston' II: On the Nature of Heat, Foundations of Chemistry, 2015, 17. In this early work, Lavoisier calls it “igneous fluid”.The 1880 edition of A Guide to the Scientific Knowledge of Things Familiar, a 19th-century educational science book, explained heat transfer in terms of the flow of caloric. In 1804, Sir John Leslie observed that a matte black surface radiates heat more effectively than a polished surface, suggesting the importance of black body radiation. In 1808, John Dalton defended caloric theory in A New System of Chemistry and described how it combines with matter, especially gases; he proposed that the heat capacity of gases varies inversely with atomic weight. In 1824, Sadi Carnot analyzed the efficiency of steam engines using caloric theory; he developed the notion of a reversible process and, in postulating that no such thing exists in nature, laid the foundation for the second law of thermodynamics.

Research into cyclones and air flow

(File:Earth Global Circulation - en.svg|thumb|300px|General Circulation of the Earth's Atmosphere: The westerlies and trade winds are part of the Earth's atmospheric circulation)In 1494, Christopher Columbus experienced a tropical cyclone, which led to the first written European account of a hurricane.Morison, Samuel Eliot, Admiral of the Ocean Sea: A Life of Cristopher Columbus, Boston, 1942, page 617. In 1686, Edmund Halley presented a systematic study of the trade winds and monsoons and identified solar heating as the cause of atmospheric motions.Cook, Alan H., Edmond Halley: Charting the Heavens and the Seas (Oxford: Clarendon Press, 1998) In 1735, an ideal explanation of global circulation through study of the trade winds was written by George Hadley.George Hadley, "Concerning the cause of the general trade winds," Philosophical Transactions, vol. 39 (1735). In 1743, when Benjamin Franklin was prevented from seeing a lunar eclipse by a hurricane, he decided that cyclones move in a contrary manner to the winds at their periphery.Dorst, Neal, FAQ:_Hurricanes,_Typhoons,_and_Tropical_Cyclones:_Hurricane_Timeline, Hurricane_Research_Division,_Atlantic_Oceanographic_and_Meteorological_Laboratory,_NOAA, January 2006. Understanding the kinematics of how exactly the rotation of the Earth affects airflow was partial at first. Gaspard-Gustave Coriolis published a paper in 1835 on the energy yield of machines with rotating parts, such as waterwheels.JOURNAL, G-G Coriolis, Sur les équations du mouvement relatif des systèmes de corps, J. De l'Ecole royale polytechnique, 15, 144–154, 1835, In 1856, William Ferrel proposed the existence of a circulation cell in the mid-latitudes, and the air within deflected by the Coriolis force resulting in the prevailing westerly winds.William Ferrel. An Essay on the Winds and the Currents of the Ocean. {{webarchive|url=https://web.archive.org/web/20131011124201weblink |date=2013-10-11 }} Retrieved on 2009-01-01. Late in the 19th century, the motion of air masses along isobars was understood to be the result of the large-scale interaction of the pressure gradient force and the deflecting force. By 1912, this deflecting force was named the Coriolis effect.BOOK, The Dynamics of Particles and of Rigid, Elastic, and Fluid Bodies, Arthur Gordon Webster, B.G. Teubner, 1912, 320,weblink Just after World War I, a group of meteorologists in Norway led by Vilhelm Bjerknes developed the Norwegian cyclone model that explains the generation, intensification and ultimate decay (the life cycle) of mid-latitude cyclones, and introduced the idea of fronts, that is, sharply defined boundaries between air masses.Shaye Johnson. The Norwegian Cyclone Model. {{webarchive|url=https://web.archive.org/web/20060901163934weblink |date=2006-09-01 }} Retrieved on 2006-10-11. The group included Carl-Gustaf Rossby (who was the first to explain the large scale atmospheric flow in terms of fluid dynamics), Tor Bergeron (who first determined how rain forms) and Jacob Bjerknes.

Observation networks and weather forecasting

(File:Wolkenstockwerke.png|thumb|300px|Cloud classification by altitude of occurrence)File:Hyetographic_or_Rain_Map_of_the_World_1848_Alexander_Keith_Johnston.png|thumb|300px|right|This "Hyetographic or Rain Map of the World " was first published 1848 by Alexander Keith Johnston ]](File:Hyetographic_or_Rain_Map_of_Europe_1848_Alexander_Keith_Johnston.png|thumb|300px|right|This "Hyetographic or Rain Map of Europe" was also published in 1848 as part of "The Physical Atlas"){{See also|History of surface weather analysis}}In the late 16th century and first half of the 17th century a range of meteorological instruments were invented - the thermometer, barometer, hydrometer, as well as wind and rain gauges. In the 1650s natural philosophers started using these instruments to systematically record weather observations. Scientific academies established weather diaries and organised observational networks.BOOK, The Oxford Companion to the History of Modern Science, Oxford University Press, 2003, John L. Heilbron, 9780199743766, 518, In 1654, Ferdinando II de Medici established the first weather observing network, that consisted of meteorological stations in Florence, Cutigliano, Vallombrosa, Bologna, Parma, Milan, Innsbruck, Osnabrück, Paris and Warsaw. The collected data were sent to Florence at regular time intervals.Raymond S. Bradley, Philip D. Jones, Climate Since A.D. 1500, Routledge, 1992, {{ISBN|0-415-07593-9}}, p.144 In the 1660s Robert Hooke of the Royal Society of London sponsored networks of weather observers. Hippocrates' treatise Airs, Waters, and Places had linked weather to disease. Thus early meteorologists attempted to correlate weather patterns with epidemic outbreaks, and the climate with public health. During the Age of Enlightenment meteorology tried to rationalise traditional weather lore, including astrological meteorology. But there were also attempts to establish a theoretical understanding of weather phenomena. Edmond Halley and George Hadley tried to explain trade winds. They reasoned that the rising mass of heated equator air is replaced by an inflow of cooler air from high latitudes. A flow of warm air at high altitude from equator to poles in turn established an early picture of circulation. Frustration with the lack of discipline among weather observers, and the poor quality of the instruments, led the early modern nation states to organise large observation networks. Thus by the end of the 18th century meteorologists had access to large quantities of reliable weather date. In 1832, an electromagnetic telegraph was created by Baron Schilling.Rebecca Martin (2009) Catapult - Indepth - Communication: telegraph, Australian Broadcasting Corporation, Retrieved on 2009-05-12 The arrival of the electrical telegraph in 1837 afforded, for the first time, a practical method for quickly gathering surface weather observations from a wide area.Library of Congress, The Invention of the Telegraph, Retrieved on 2009-01-01This data could be used to produce maps of the state of the atmosphere for a region near the Earth's surface and to study how these states evolved through time. To make frequent weather forecasts based on these data required a reliable network of observations, but it was not until 1849 that the Smithsonian Institution began to establish an observation network across the United States under the leadership of Joseph Henry.WEB,weblink Smithsonian Institution Archives, Smithsonian Institution Archives, 16 June 2015, yes,weblink" title="web.archive.org/web/20061020020548weblink">weblink 20 October 2006, Similar observation networks were established in Europe at this time. The Reverend William Clement Ley was key in understanding of cirrus clouds and early understandings of Jet Streams.WEB,weblink Prophet without Honour: The Reverend William Clement Ley and the hunt for the jet stream, rmets.org, 13 October 2016, Charles Kenneth Mackinnon Douglas, known as 'CKM' Douglas read Ley's papers after his death and carried on the early study of weather systems.JOURNAL,weblink Meteorologist's profile — Charles Kenneth Mackinnon Douglas, OBE, AFC, MA, M., Field, 1 October 1999, 54, 10, 321–327, 13 October 2016, Wiley Online Library, 10.1002/j.1477-8696.1999.tb03992.x, 1999Wthr...54..321F, Nineteenth century researchers in meteorology were drawn from military or medical backgrounds, rather than trained as dedicated scientists.JOURNAL, Williamson, Fiona, 2015-09-01, Weathering the empire: meteorological research in the early British straits settlements,weblink The British Journal for the History of Science, 48, 3, 475–492, 10.1017/S000708741500028X, 1474-001X, In 1854, the United Kingdom government appointed Robert FitzRoy to the new office of Meteorological Statist to the Board of Trade with the task of gathering weather observations at sea. FitzRoy's office became the United Kingdom Meteorological Office in 1854, the second oldest national meteorological service in the world (the Central Institution for Meteorology and Geodynamics (ZAMG) in Austria was founded in 1851 and is the oldest weather service in the world). The first daily weather forecasts made by FitzRoy's Office were published in The Times newspaper in 1860. The following year a system was introduced of hoisting storm warning cones at principal ports when a gale was expected.Over the next 50 years many countries established national meteorological services. The India Meteorological Department (1875) was established to follow tropical cyclone and monsoon.India Meteorological Department Establishment of IMD. {{webarchive|url=https://web.archive.org/web/20151120224108weblink |date=2015-11-20 }} Retrieved on 2009-01-01. The Finnish Meteorological Central Office (1881) was formed from part of Magnetic Observatory of Helsinki University.Finnish Meteorological Institute. History of Finnish Meteorological Institute. {{webarchive|url=https://web.archive.org/web/20100725213620weblink |date=2010-07-25 }} Retrieved on 2009-01-01. Japan's Tokyo Meteorological Observatory, the forerunner of the Japan Meteorological Agency, began constructing surface weather maps in 1883.Japan Meteorological Agency. History. {{webarchive|url=https://web.archive.org/web/20101225034901weblink |date=2010-12-25 }} Retrieved on 2006-10-22. The United States Weather Bureau (1890) was established under the United States Department of Agriculture. The Australian Bureau of Meteorology (1906) was established by a Meteorology Act to unify existing state meteorological services.WEB,weblink BOM celebrates 100 years, Australian Broadcasting Corporation, 2008-01-01, WEB, Collections in Perth: 20. Meteorology, National Archives of Australia,weblink 2008-05-24,

Numerical weather prediction

(File:IBM 7090 console used by a meteorologist, 1965.jpg|thumb|A meteorologist at the console of the IBM 7090 in the Joint Numerical Weather Prediction Unit. c. 1965)In 1904, Norwegian scientist Vilhelm Bjerknes first argued in his paper Weather Forecasting as a Problem in Mechanics and Physics that it should be possible to forecast weather from calculations based upon natural laws.Berknes, V. (1904) "Das Problem der Wettervorhersage, betrachtet vom Standpunkte der Mechanik und der Physik" (The problem of weather prediction, considered from the viewpoints of mechanics and physics), Meteorologische Zeitschrift, 21 : 1–7. Available in English on-line at: Schweizerbart science publishers.WEB,weblink PDF, Pioneers in Modern Meteorology and Climatology: Vilhelm and Jacob Bjerknes, 2008-10-13, It was not until later in the 20th century that advances in the understanding of atmospheric physics led to the foundation of modern numerical weather prediction. In 1922, Lewis Fry Richardson published "Weather Prediction By Numerical Process",Richardson, Lewis Fry, Weather Prediction by Numerical Process (Cambridge, England: Cambridge University Press, 1922). Available on-line at: Internet Archive.org. after finding notes and derivations he worked on as an ambulance driver in World War I. He described how small terms in the prognostic fluid dynamics equations that govern atmospheric flow could be neglected, and a numerical calculation scheme that could be devised to allow predictions. Richardson envisioned a large auditorium of thousands of people performing the calculations. However, the sheer number of calculations required was too large to complete without electronic computers, and the size of the grid and time steps used in the calculations led to unrealistic results. Though numerical analysis later found that this was due to numerical instability.Starting in the 1950s, numerical forecasts with computers became feasible.American Institute of Physics. Atmospheric General Circulation Modeling. {{webarchive|url=https://web.archive.org/web/20080325084036weblink |date=2008-03-25 }} Retrieved on 2008-01-13. The first weather forecasts derived this way used barotropic (single-vertical-level) models, and could successfully predict the large-scale movement of midlatitude Rossby waves, that is, the pattern of atmospheric lows and highs.BOOK, Storm Watchers, 208, 2002, Cox, John D., John Wiley & Sons, Inc., 0-471-38108-X, In 1959, the UK Meteorological Office received its first computer, a Ferranti Mercury. WEB,weblink The history of Numerical Weather Prediction at the Met Office, Met Office, In the 1960s, the chaotic nature of the atmosphere was first observed and mathematically described by Edward Lorenz, founding the field of chaos theory.Edward N. Lorenz, "Deterministic non-periodic flow", Journal of the Atmospheric Sciences, vol. 20, pages 130–141 (1963). These advances have led to the current use of ensemble forecasting in most major forecasting centers, to take into account uncertainty arising from the chaotic nature of the atmosphere.WEB,weblink Manousos, Peter, Hydrometeorological Prediction Center, 2006-07-19, 2010-12-31, Ensemble Prediction Systems, Mathematical models used to predict the long term weather of the Earth (climate models), have been developed that have a resolution today that are as coarse as the older weather prediction models. These climate models are used to investigate long-term climate shifts, such as what effects might be caused by human emission of greenhouse gases.

Meteorologists

{{further|Weather forecasting}}Meteorologists are scientists who study meteorology.BOOK, Todd S., Glickman, Cambridge, Massachusetts, June 2009,weblink Meteorology Glossary, electronic, 2nd, American Meteorological Society, March 10, 2014, The American Meteorological Society published and continually updates an authoritative electronic Meteorology Glossary.BOOK, Todd S., Glickman, Cambridge, Massachusetts, June 2000,weblink Meteorology Glossary, electronic, 2nd, American Meteorological Society, March 10, 2014, Meteorologists work in government agencies, private consulting and research services, industrial enterprises, utilities, radio and television stations, and in education. In the United States, meteorologists held about 9,400 jobs in 2009.Bureau of labor statistics: "Occupational Outlook Handbook, 2010-11 Edition"Meteorologists are best known by the public for weather forecasting. Some radio and television weather forecasters are professional meteorologists, while others are reporters (weather specialist, weatherman, etc.) with no formal meteorological training. The American Meteorological Society and National Weather Association issue "Seals of Approval" to weather broadcasters who meet certain requirements.

Equipment

File:Huracán Hugo.jpg|thumb|Satellite image of Hurricane Hugo with a polar lowpolar lowEach science has its own unique sets of laboratory equipment. In the atmosphere, there are many things or qualities of the atmosphere that can be measured. Rain, which can be observed, or seen anywhere and anytime was one of the first atmospheric qualities measured historically. Also, two other accurately measured qualities are wind and humidity. Neither of these can be seen but can be felt. The devices to measure these three sprang up in the mid-15th century and were respectively the rain gauge, the anemometer, and the hygrometer. Many attempts had been made prior to the 15th century to construct adequate equipment to measure the many atmospheric variables. Many were faulty in some way or were simply not reliable. Even Aristotle noted this in some of his work as the difficulty to measure the air.Sets of surface measurements are important data to meteorologists. They give a snapshot of a variety of weather conditions at one single location and are usually at a weather station, a ship or a weather buoy. The measurements taken at a weather station can include any number of atmospheric observables. Usually, temperature, pressure, wind measurements, and humidity are the variables that are measured by a thermometer, barometer, anemometer, and hygrometer, respectively.Office of the Federal Coordinator of Meteorology. Federal Meteorological Handbook No. 1 - Surface Weather Observations and Reports: September 2005. {{webarchive|url=https://web.archive.org/web/19990420051036weblink |date=1999-04-20 }} Retrieved on 2009-01-02. Professional stations may also include air quality sensors (carbon monoxide, carbon dioxide, methane, ozone, dust, and smoke), ceilometer (cloud ceiling), falling precipitation sensor, flood sensor, lightning sensor, microphone (explosions, sonic booms, thunder), pyranometer/pyrheliometer/spectroradiometer (IR/Vis/UV photodiodes), rain gauge/snow gauge, scintillation counter (background radiation, fallout, radon), seismometer (earthquakes and tremors), transmissometer (visibility), and a GPS clock for data logging. Upper air data are of crucial importance for weather forecasting. The most widely used technique is launches of radiosondes. Supplementing the radiosondes a network of aircraft collection is organized by the World Meteorological Organization.Remote sensing, as used in meteorology, is the concept of collecting data from remote weather events and subsequently producing weather information. The common types of remote sensing are Radar, Lidar, and satellites (or photogrammetry). Each collects data about the atmosphere from a remote location and, usually, stores the data where the instrument is located. Radar and Lidar are not passive because both use EM radiation to illuminate a specific portion of the atmosphere.Peebles, Peyton, [1998], Radar Principles, John Wiley & Sons, Inc., New York, {{ISBN|0-471-25205-0}}. Weather satellites along with more general-purpose Earth-observing satellites circling the earth at various altitudes have become an indispensable tool for studying a wide range of phenomena from forest fires to El Niño.

Spatial scales

The study of the atmosphere can be divided into distinct areas that depend on both time and spatial scales. At one extreme of this scale is climatology. In the timescales of hours to days, meteorology separates into micro-, meso-, and synoptic scale meteorology. Respectively, the geospatial size of each of these three scales relates directly with the appropriate timescale.Other subclassifications are used to describe the unique, local, or broad effects within those subclasses.{| class="wikitable" style="border-spacing: 5px; margin:auto;"Typical Scales of Atmospheric Motion SystemsHOLTON, James, An Introduction to Dynamic Meteorology,weblink Elsevier Academic Press, 5 March 2016, 5, ! scope="col" style="width:150px;"| Type of motion! scope="col" style="width:100px;"| Horizontal scale (meter)
| 10−3
| 10−2 - 10−1
| 10−1 - 1
| 1 - 10
| 10 - 102
| 102
| 103
| 104 - 105
| 105
| 106
| 107
| 107
| 107

Microscale

Microscale meteorology is the study of atmospheric phenomena on a scale of about {{convert|1|km|mi}} or less. Individual thunderstorms, clouds, and local turbulence caused by buildings and other obstacles (such as individual hills) are modeled on this scale.WEB,weblink AMS Glossary of Meteorology, 2008-04-12, American Meteorological Society, yes,weblink" title="web.archive.org/web/20110606101802weblink">weblink 2011-06-06,

Mesoscale

Mesoscale meteorology is the study of atmospheric phenomena that has horizontal scales ranging from 1 km to 1000 km and a vertical scale that starts at the Earth's surface and includes the atmospheric boundary layer, troposphere, tropopause, and the lower section of the stratosphere. Mesoscale timescales last from less than a day to weeks. The events typically of interest are thunderstorms, squall lines, fronts, precipitation bands in tropical and extratropical cyclones, and topographically generated weather systems such as mountain waves and sea and land breezes.Online Glossary of Meteorology, American Meteorological Society weblink, 2nd Ed., 2000, Allen Press.

Synoptic scale

File:Surface analysis.gif|thumb|300px|(NOAA]]: Synoptic scale weather analysis.)Synoptic scale meteorology predicts atmospheric changes at scales up to 1000 km and 105 sec (28 days), in time and space. At the synoptic scale, the Coriolis acceleration acting on moving air masses (outside of the tropics) plays a dominant role in predictions. The phenomena typically described by synoptic meteorology include events such as extratropical cyclones, baroclinic troughs and ridges, frontal zones, and to some extent jet streams. All of these are typically given on weather maps for a specific time. The minimum horizontal scale of synoptic phenomena is limited to the spacing between surface observation stations.Bluestein, H., Synoptic-Dynamic Meteorology in Midlatitudes: Principles of Kinematics and Dynamics, Vol. 1, Oxford University Press, 1992; {{ISBN|0-19-506267-1}}

Global scale

(File:WOA09 sea-surf TMP AYool.png|thumb|300px|Annual mean sea surface temperatures.)Global scale meteorology is the study of weather patterns related to the transport of heat from the tropics to the poles. Very large scale oscillations are of importance at this scale. These oscillations have time periods typically on the order of months, such as the Madden–Julian oscillation, or years, such as the El Niño–Southern Oscillation and the Pacific decadal oscillation. Global scale meteorology pushes into the range of climatology. The traditional definition of climate is pushed into larger timescales and with the understanding of the longer time scale global oscillations, their effect on climate and weather disturbances can be included in the synoptic and mesoscale timescales predictions.Numerical Weather Prediction is a main focus in understanding air–sea interaction, tropical meteorology, atmospheric predictability, and tropospheric/stratospheric processes.Global Modelling, US Naval Research Laboratory, Monterey, Ca. The Naval Research Laboratory in Monterey, California, developed a global atmospheric model called Navy Operational Global Atmospheric Prediction System (NOGAPS). NOGAPS is run operationally at Fleet Numerical Meteorology and Oceanography Center for the United States Military. Many other global atmospheric models are run by national meteorological agencies.

Some meteorological principles

Boundary layer meteorology

Boundary layer meteorology is the study of processes in the air layer directly above Earth's surface, known as the atmospheric boundary layer (ABL). The effects of the surface â€“ heating, cooling, and friction â€“ cause turbulent mixing within the air layer. Significant movement of heat, matter, or momentum on time scales of less than a day are caused by turbulent motions.Garratt, J.R., The atmospheric boundary layer'', Cambridge University Press, 1992; {{ISBN|0-521-38052-9}}. Boundary layer meteorology includes the study of all types of surface–atmosphere boundary, including ocean, lake, urban land and non-urban land for the study of meteorology.

Dynamic meteorology

Dynamic meteorology generally focuses on the fluid dynamics of the atmosphere. The idea of air parcel is used to define the smallest element of the atmosphere, while ignoring the discrete molecular and chemical nature of the atmosphere. An air parcel is defined as a point in the fluid continuum of the atmosphere. The fundamental laws of fluid dynamics, thermodynamics, and motion are used to study the atmosphere. The physical quantities that characterize the state of the atmosphere are temperature, density, pressure, etc. These variables have unique values in the continuum.Holton, J.R. [2004]. An Introduction to Dynamic Meteorology, 4th Ed., Burlington, Md: Elsevier Inc.. {{ISBN|0-12-354015-1}}.

Applications

Weather forecasting

(File:Day5pressureforecast.png|thumb|300px|Forecast of surface pressures five days into the future for the north Pacific, North America, and north Atlantic Ocean)Weather forecasting is the application of science and technology to predict the state of the atmosphere at a future time and given location. Humans have attempted to predict the weather informally for millennia and formally since at least the 19th century.Mistic House, Astrology Lessons, History, Prediction, Skeptics, and Astrology Compatibility, Retrieved on 2008-01-12, Archived at: {{webarchive |url=https://web.archive.org/web/20080608133837weblink |date=June 8, 2008 }}Eric D. Craft, An Economic History of Weather Forecasting {{webarchive|url=https://web.archive.org/web/20070503193324weblink |date=2007-05-03 }}, Retrieved on 2007-04-15 Weather forecasts are made by collecting quantitative data about the current state of the atmosphere and using scientific understanding of atmospheric processes to project how the atmosphere will evolve.NASA, Weather Forecasting Through the Ages, Retrieved on 2008-05-25Once an all-human endeavor based mainly upon changes in barometric pressure, current weather conditions, and sky condition,Weather Doctor, Applying The Barometer To Weather Watching, Retrieved on 2008-05-25Mark Moore, Field Forecasting - A Short Summary {{webarchive|url=https://web.archive.org/web/20090325034756weblink |date=2009-03-25 }}, Retrieved on 2008-05-25 forecast models are now used to determine future conditions. Human input is still required to pick the best possible forecast model to base the forecast upon, which involves pattern recognition skills, teleconnections, knowledge of model performance, and knowledge of model biases. The chaotic nature of the atmosphere, the massive computational power required to solve the equations that describe the atmosphere, error involved in measuring the initial conditions, and an incomplete understanding of atmospheric processes mean that forecasts become less accurate as the difference in current time and the time for which the forecast is being made (the range of the forecast) increases. The use of ensembles and model consensus help narrow the error and pick the most likely outcome.Klaus Weickmann, Jeff Whitaker, Andres Roubicek and Catherine Smith. The Use of Ensemble Forecasts to Produce Improved Medium Range (3-15 days) Weather Forecasts. Retrieved on 2007-02-16.Todd Kimberlain. Tropical cyclone motion and intensity talk (June 2007). Retrieved on 2007-07-21.Richard J. Pasch, Mike Fiorino, and Chris Landsea. TPC/NHC’S REVIEW OF THE NCEP PRODUCTION SUITE FOR 2006.{{dead link|date=January 2018 |bot=InternetArchiveBot |fix-attempted=yes }} Retrieved on 2008-05-05.There are a variety of end uses to weather forecasts. Weather warnings are important forecasts because they are used to protect life and property.National Weather Service Mission Statement {{webarchive|url=https://web.archive.org/web/20131124214601weblink |date=2013-11-24 }}, Retrieved on 2008-05-25 Forecasts based on temperature and precipitation are important to agriculture,Blair Fannin, Dry weather conditions continue for Texas {{webarchive|url=https://web.archive.org/web/20090703095038weblink |date=2009-07-03 }}, Retrieved on 2008-05-26Dr. Terry Mader, Drought Corn Silage {{webarchive|url=https://web.archive.org/web/20111005203246weblink |date=2011-10-05 }}, Retrieved on 2008-05-26Kathryn C. Taylor, Peach Orchard Establishment and Young Tree Care {{webarchive|url=https://web.archive.org/web/20081224112403weblink |date=2008-12-24 }}, Retrieved on 2008-05-26Associated Press, After Freeze, Counting Losses to Orange Crop, Retrieved on 2008-05-26 and therefore to commodity traders within stock markets. Temperature forecasts are used by utility companies to estimate demand over coming days.The New York Times, FUTURES/OPTIONS; Cold Weather Brings Surge In Prices of Heating Fuels, Retrieved on 2008-05-25BBC, Heatwave causes electricity surge, Retrieved on 2008-05-25The Seven Key Messages of the Energy Drill Program {{webarchive|url=https://web.archive.org/web/20120217042744weblink |date=2012-02-17 }}, Retrieved on 2008-05-25 On an everyday basis, people use weather forecasts to determine what to wear. Since outdoor activities are severely curtailed by heavy rain, snow, and wind chill, forecasts can be used to plan activities around these events, and to plan ahead and survive them.

Aviation meteorology

Aviation meteorology deals with the impact of weather on air traffic management. It is important for air crews to understand the implications of weather on their flight plan as well as their aircraft, as noted by the Aeronautical Information Manual:An international version called the Aeronautical Information Publication contains parallel information, as well as specific information on the international airports for use by the international community.The effects of ice on aircraft are cumulative—thrust is reduced, drag increases, lift lessens, and weight increases. The results are an increase in stall speed and a deterioration of aircraft performance. In extreme cases, 2 to 3 inches of ice can form on the leading edge of the airfoil in less than 5 minutes. It takes but 1/2 inch of ice to reduce the lifting power of some aircraft by 50 percent and increases the frictional drag by an equal percentage."7-1-22. PIREPs Relating to Airframe Icing", [February 16, 2006], Aeronautical Information Manual, FAA AIM Online {{webarchive|url=https://web.archive.org/web/20090712031134weblink |date=2009-07-12 }}

Agricultural meteorology

Meteorologists, soil scientists, agricultural hydrologists, and agronomists are persons concerned with studying the effects of weather and climate on plant distribution, crop yield, water-use efficiency, phenology of plant and animal development, and the energy balance of managed and natural ecosystems. Conversely, they are interested in the role of vegetation on climate and weather.Agricultural and Forest Meteorology, Elsevier, {{ISSN|0168-1923}}.

Hydrometeorology

Hydrometeorology is the branch of meteorology that deals with the hydrologic cycle, the water budget, and the rainfall statistics of storms.Encyclopædia Britannica, 2007. A hydrometeorologist prepares and issues forecasts of accumulating (quantitative) precipitation, heavy rain, heavy snow, and highlights areas with the potential for flash flooding. Typically the range of knowledge that is required overlaps with climatology, mesoscale and synoptic meteorology, and other geosciences.About the HPC, NOAA/ National Weather Service, National Centers for Environmental Prediction, Hydrometeorological Prediction Center, Camp Springs, Maryland, 2007.The multidisciplinary nature of the branch can result in technical challenges, since tools and solutions from each of the individual disciplines involved may behave slightly differently, be optimized for different hard- and software platforms and use different data formats. There are some initiatives - such as the DRIHM projectWEB,weblink Home, Super User, 16 June 2015, - that are trying to address this issue.DRIHM News, number 1, March 2012, p2 "An ideal environment for hydro-meteorology research at the European level"

Nuclear meteorology

Nuclear meteorology investigates the distribution of radioactive aerosols and gases in the atmosphere.WEB,weblink Modern research in nuclear meteorology, July 6, 2008, February 1974, PDF, Atomic Energy, Springer New York, 10.1007/BF01117823,

Maritime meteorology

Maritime meteorology deals with air and wave forecasts for ships operating at sea. Organizations such as the Ocean Prediction Center, Honolulu National Weather Service forecast office, United Kingdom Met Office, and JMA prepare high seas forecasts for the world's oceans.

Military meteorology

Military meteorology is the research and application of meteorology for military purposes. In the United States, the United States Navy's Commander, Naval Meteorology and Oceanography Command oversees meteorological efforts for the Navy and Marine Corps while the United States Air Force's Air Force Weather Agency is responsible for the Air Force and Army.

Environmental meteorology

Environmental meteorology mainly analyzes industrial pollution dispersion physically and chemically based on meteorological parameters such as temperature, humidity, wind, and various weather conditions.

Renewable energy

Meteorology applications in renewable energy includes basic research, "exploration", and potential mapping of wind power and solar radiation for wind and solar energy.

See also

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References

{{Reflist}}

Further reading

  • Byers, Horace. General Meteorology. New York: McGraw-Hill, 1994.
  • BOOK, Garret, J.R., The atmospheric boundary layer, Cambridge University Press, 0-521-38052-9, 1992, 1992,
  • BOOK,weblink American Meteorological Society, Glossary of Meteorology,weblink 2nd, Allen Press, 2000,
  • BOOK, Bluestein, H, Synoptic-Dynamic Meteorology in Midlatitudes: Principles of Kinematics and Dynamics, Vol. 1, Oxford University Press, 0-19-506267-1, 1992, 1992,
  • BOOK, Bluestein, H, Synoptic-Dynamic Meteorology in Midlatitudes: Volume II: Observations and Theory of Weather Systems, Oxford University Press, 0-19-506268-X, 1993, 1993,
  • BOOK, Reynolds, R, Guide to Weather, Firefly Books Inc, Buffalo, New York, 1-55407-110-0, 208, 2005, 2005,
  • BOOK, Holton, J.R., An Introduction to Dynamic Meteorology,weblink 4th, Elsevier Inc., Burlington, Md, 0-12-354015-1, 2004, 2004,
  • BOOK, Roulstone, Ian, Norbury, John, yes, Invisible in the Storm: the role of mathematics in understanding weather,weblink 2013, Princeton University Press,

Dictionaries and encyclopedias

  • BOOK, Todd S., Glickman, Cambridge, Massachusetts, June 2000,weblink Meteorology Glossary, electronic, 2nd, American Meteorological Society,
  • BOOK, Roberto, Gustavo Herrera, Ricardo, García-Herrera, Luis, Prieto, David, Gallego, Emiliano, Hernández, Luis, Gimeno, Gunther, Können, Frits, Koek, Dennis, Wheeler, Clive, Wilkinson, Maria, Del Rosario Prieto, Carlos, Báez, Scott, Woodruff,weblink A Dictionary of Nautical Meteorological Terms: CLIWOC Multilingual Dictionary of Meteorological Terms; An English/Spanish/French/Dutch Dictionary of Windforce Terms Used by Mariners from 1750 to 1850, CLIWOC, PDF,
  • WEB,weblink Meteorology Encyclopedia, Central Weather Bureau,

External links

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