Timeline of meteorology

Source: Wikipedia, the free encyclopedia.

The timeline of meteorology contains events of scientific and technological advancements in the area of

atmospheric sciences. The most notable advancements in observational meteorology, weather forecasting, climatology, atmospheric chemistry, and atmospheric physics
are listed chronologically. Some historical weather events are included that mark time periods where advancements were made, or even that sparked policy change.

Antiquity

  • 3000 BC – Meteorology in India can be traced back to around 3000 BC, with writings such as the Upanishads, containing discussions about the processes of cloud formation and rain and the seasonal cycles caused by the movement of earth round the sun.[1]
  • 600 BC –
    Thales
    may qualify as the first Greek meteorologist. He reputedly issues the first seasonal crop forecast.
  • 400 BC – There is some evidence that Democritus predicted changes in the weather, and that he used this ability to convince people that he could predict other future events.[2]
  • 400 BC – Hippocrates writes a treatise called Airs, Waters and Places, the earliest known work to include a discussion of weather. More generally, he wrote about common diseases that occur in particular locations, seasons, winds and air.[2]
  • 350 BC – The Greek philosopher Aristotle writes Meteorology, a work which represents the sum of knowledge of the time about earth sciences, including weather and climate. It is the first known work that attempts to treat a broad range of meteorological topics.[3] For the first time, precipitation and the clouds from which precipitation falls are called meteors, which originate from the Greek word meteoros, meaning 'high in the sky'. From that word comes the modern term meteorology, the study of clouds and weather.
Although the term meteorology is used today to describe a subdiscipline of the atmospheric sciences, Aristotle's work is more general. Meteorologica is based on intuition and simple observation, but not on what is now considered the scientific method. In his own words:
...all the affections we may call common to air and water, and the kinds and parts of the earth and the affections of its parts.[4]
The magazine
De Mundo (attributed to Pseudo-Aristotle) notes:[5]
Cloud is a vaporous mass, concentrated and producing water. Rain is produced from the compression of a closely condensed cloud, varying according to the pressure exerted on the cloud; when the pressure is slight it scatters gentle drops; when it is great it produces a more violent fall, and we call this a shower, being heavier than ordinary rain, and forming continuous masses of water falling over earth. Snow is produced by the breaking up of condensed clouds, the cleavage taking place before the change into water; it is the process of cleavage which causes its resemblance to foam and its intense whiteness, while the cause of its coldness is the congelation of the moisture in it before it is dispersed or rarefied. When snow is violent and falls heavily we call it a blizzard. Hail is produced when snow becomes densified and acquires impetus for a swifter fall from its close mass; the weight becomes greater and the fall more violent in proportion to the size of the broken fragments of cloud. Such then are the phenomena which occur as the result of moist exhalation.
One of the most impressive achievements in
hydrologic cycle
:
Now the sun, moving as it does, sets up processes of change and becoming and decay, and by its agency the finest and sweetest water is every day carried up and is dissolved into vapour and rises to the upper region, where it is condensed again by the cold and so returns to the earth.[4]
Aristotle
  • Several years after Aristotle's book, his pupil Theophrastus puts together a book on weather forecasting called The Book of Signs. Various indicators such as solar and lunar halos formed by high clouds are presented as ways to forecast the weather. The combined works of Aristotle and Theophrastus have such authority they become the main influence in the study of clouds, weather and weather forecasting for nearly 2000 years.[3]
  • 250 BC –
    cumulonimbus).[2]
  • 25 AD –
    Roman empire, formalizes the climatic zone system.[6]
  • c. 80 AD – In his Lunheng (論衡; Critical Essays), the Han dynasty Chinese philosopher Wang Chong (27–97 AD) dispels the Chinese myth of rain coming from the heavens, and states that rain is evaporated from water on the earth into the air and forms clouds, stating that clouds condense into rain and also form dew, and says when the clothes of people in high mountains are moistened, this is because of the air-suspended rain water.[7] However, Wang Chong supports his theory by quoting a similar one of Gongyang Gao's,[7] the latter's commentary on the Spring and Autumn Annals, the Gongyang Zhuan, compiled in the 2nd century BC,[7] showing that the Chinese conception of rain evaporating and rising to form clouds goes back much farther than Wang Chong. Wang Chong wrote:
As to this coming of rain from the mountains, some hold that the clouds carry the rain with them, dispersing as it is precipitated (and they are right). Clouds and rain are really the same thing. Water evaporating upwards becomes clouds, which condense into rain, or still further into dew.[7]

Middle Ages

Anemometers
  • 1450 –
    Leone Battista Alberti developed a swinging-plate anemometer, and is known as the first anemometer.[22]
– Nicolas Cryfts, (
Nicolas of Cusa), described the first hair hygrometer to measure humidity. The design was drawn by Leonardo da Vinci, referencing Cryfts design in da Vinci's Codex Atlanticus.[22]
  • 1483 − Yuriy Drohobych publishes Prognostic Estimation of the year 1483 in Rome, where he reflects upon weather forecasting and that climatic conditions depended on the latitude.[23]
  • 1488 – Johannes Lichtenberger publishes the first version of his Prognosticatio linking weather forecasting with astrology. The paradigm was only challenged centuries later.[24]
  • 1494 – During his second voyage Christopher Columbus experiences a tropical cyclone in the Atlantic Ocean, which leads to the first written European account of a hurricane.[25][26]
  • 1510 – Leonhard Reynmann, astronomer of Nuremberg, publishes ″Wetterbüchlein Von warer erkanntnus des wetters″, a collection of weather lore.[27][28]
  • 1547 − Antonio Mizauld publishes "Le miroueer du temps, autrement dit, éphémérides perpétuelles de l'air par lesquelles sont tous les jours donez vrais signes de touts changements de temps, seulement par choses qui à tous apparoissent au cien, en l'air, sur terre & en l'eau. Le tout par petits aphorismes, & breves sentences diligemment compris" in Paris, with detail on forecasting weather, comets and earthquakes.[29]

17th century

Galileo.
  • 1607 – Galileo Galilei constructs a thermoscope. Not only did this device measure temperature, but it represented a paradigm shift. Up to this point, heat and cold were believed to be qualities of Aristotle's elements (fire, water, air, and earth). Note: There is some controversy about who actually built this first thermoscope. There is some evidence for this device being independently built at several different times. This is the era of the first recorded meteorological observations. As there was no standard measurement, they were of little use until the work of Daniel Gabriel Fahrenheit and Anders Celsius in the 18th century.
Sir Francis Bacon
Blaise Pascal.
– Edmund Halley establishes the relationship between barometric pressure and height above sea level.[35]

18th century

Global circulation as described by Hadley.
- Royal Society begins twice daily observations compiled by Samuel Horsley testing for the influence of winds and of the moon on the barometer readings.[43]
– First hair
Horace-Bénédict de Saussure
.

19th century

Isothermal chart of the world created 1823 by William Channing Woodbridge using the work of Alexander von Humboldt.
  • 1800 – The Voltaic pile was the first modern electric battery, invented by Alessandro Volta, which led to later inventions like the telegraph.
  • 1802–1803 –
    nimbus, taken from the Latin word for rain cloud,[49] is given to complex systems of cirriform, cumuliform, and stratiform clouds with sufficient vertical development to produce significant precipitation,[51][52] and it comes to be identified as a distinct nimbiform physical category.[53]
Classification of major types: 1803 Stratiform Cirriform Cumulostratiform Cumuliform Nimbiform
Upper-level Cirrostratus Cirrus Cirrocumulus
Lower-level Stratus Cumulus
Multi-level/vertical Cumulostratus Nimbus
John Herapath develops some ideas in the kinetic theory of gases but mistakenly associates temperature with molecular momentum rather than kinetic energy; his work receives little attention other than from Joule.
What hath God wrought[55]
  • 1839 – The first commercial electrical telegraph was constructed by Sir William Fothergill Cooke and entered use on the Great Western Railway. Cooke and Wheatstone patented it in May 1837 as an alarm system.
  • 1840 – Elias Loomis becomes the first person known to attempt to devise a theory on frontal zones. The idea of fronts do not catch on until expanded upon by the Norwegians in the years following World War I.[56]
– German meteorologist Ludwig Kaemtz adds stratocumulus to Howard's canon as a mostly detached low-étage genus of limited convection.[57] It is defined as having cumuliform and stratiform characteristics integrated into a single layer (in contrast to cumulostratus which is deemed to be composite in nature and can be structured into more than one layer).[51] This eventually leads to the formal recognition of a stratocumuliform[58] physical category that includes rolled and rippled clouds classified separately from the more freely convective heaped cumuliform clouds.
  • 1843 – John James Waterston fully expounds the kinetic theory of gases, but is ridiculed and ignored.
James Prescott Joule experimentally finds the mechanical equivalent of heat.
– The Manchester Examiner newspaper organises the first weather reports collected by electrical means.[62]
  • 1848 –
    William Thomson
    extends the concept of absolute zero from gases to all substances.
  • 1849 – Smithsonian Institution begins to establish an observation network across the United States, with 150 observers via telegraph, under the leadership of Joseph Henry.[63]
saturated vapour pressure and temperature
using his hypothesis of molecular vortices.
  • 1850 – Rankine uses his vortex theory to establish accurate relationships between the temperature,
    saturated steam
    will be negative.
second law
of thermodynamics, abandoning the caloric theory, but preserving Carnot's principle.
– Rankine introduces his thermodynamic function, later identified as entropy.
  • Mid 1850s – Emilien Renou, director of the Parc Saint-Maur and Montsouris observatories, begins work on an elaboration of Howard's classifications that would lead to the introduction during the 1870s of a newly defined middle étage .[51] Clouds in this altitude range are given the prefix alto- derived from the Latin word altum pertaining to height above the low-level clouds. This resultes in the genus name altocumulus for mid-level cumuliform and stratocumuliform types and altostratus for stratiform types in the same altitude range.[49]
  • 1856 – William Ferrel publishes his essay on the winds and the currents of the oceans.
  • 1859 – James Clerk Maxwell discovers the distribution law of molecular velocities.
  • 1860 – Robert FitzRoy uses the new telegraph system to gather daily observations from across England and produces the first synoptic charts. He also coined the term "weather forecast" and his were the first ever daily weather forecasts to be published in this year.
– After establishment in 1849, 500 U.S. telegraph stations are now making weather observations and submitting them back to the Smithsonian Institution. The observations are later interrupted by the American Civil War.
  • 1865 –
    Josef Loschmidt
    applies Maxwell's theory to estimate the number-density of molecules in gases, given observed gas viscosities.
– Manila Observatory founded in the Philippines.[40]
– United States Army Signal Corp, forerunner of the National Weather Service, issues its first hurricane warning.[40]
Synoptic chart from 1874.
  • 1875 – The India Meteorological Department is established, after a tropical cyclone struck Calcutta in 1864 and monsoon failures during 1866 and 1871.[1]
  • 1876 –
    statistical ensembles, the free energy as the driving force behind chemical reactions, and chemical thermodynamics
    in general.
  • 1880 – Philip Weilbach, secretary and librarian at the Art Academy in Copenhagen proposes and has accepted by the permanent committee of the International Meteorological Organization (IMO), a forerunner of the present-day World Meteorological Organization (WMO), the designation of a new free-convective vertical or multi-étage genus type, cumulonimbus (heaped rain cloud). It would be distinct from cumulus and nimbus and identifiable by its often very complex structure (frequently including a cirriform top and what are now recognized as multiple accessory clouds), and its ability to produce thunder. With this addition, a canon of ten tropospheric cloud genera is established that comes to be officially and universally accepted.[51] Howard's cumulostratus is not included as a distinct type, having effectively been reclassified into its component cumuliform and stratiform genus types already included in the new canon.
  • 1881 – Finnish Meteorological Central Office was formed from part of Magnetic Observatory of
    Helsinki University
    .
  • 1890 – US
    U.S. Department of Agriculture
    .
– Otto Jesse reveals the discovery and identification of the first clouds known to form above the
noctilucent which is Latin for night shining. Because of the extremely high altitudes of these clouds in what is now known to be the mesosphere, they can become illuminated by the sun's rays when the sky is nearly dark after sunset and before sunrise.[65]
  • 1892 – William Henry Dines invented another kind of anemometer, called the pressure-tube (Dines) anemometer. His device measured the difference in pressure arising from wind blowing in a tube versus that blowing across the tube.[22]
– The first mention of the term "
El Niño" to refer to climate occurs when Captain Camilo Carrilo told the Geographical society congress in Lima that Peruvian sailors named the warm northerly current "El Niño" because it was most noticeable around Christmas
.
ice ages
.
– H.H. Clayton proposes formalizing the division of clouds by their physical structures into cirriform, stratiform, "flocciform" (stratocumuliform)[68] and cumuliform. With the later addition of cumulonimbiform, the idea eventually finds favor as an aid in the analysis of satellite cloud images.[58]
  • 1898 – US Weather Bureau established a
    hurricane warning network at Kingston, Jamaica.[40]

20th century

- The Marconi Company issues the first routine weather forecast by means of radio to ships on sea. Weather reports from ships started 1905.[70]
  • 1903 – Max Margules publishes „Über die Energie der Stürme", an essay on the atmosphere as a three-dimensional thermodynamical machine.[71]
  • 1904 – Vilhelm Bjerknes presents the vision that forecasting the weather is feasible based on mathematical methods.
  • 1905 –
    Australian Bureau of Meteorology
    established by a Meteorology Act to unify existing state meteorological services.
  • 1919 – Norwegian cyclone model introduced for the first time in meteorological literature. Marks a revolution in the way the atmosphere is conceived and immediately starts leading to improved forecasts.[72]
- Sakuhei Fujiwhara is the first to note that hurricanes move with the larger scale flow, and later publishes a paper on the Fujiwhara effect in 1921.[40]
Erik Palmén publishes his findings that hurricanes require surface water temperatures of at least 26°C (80°F) in order to form.
– Hurricanes begin to be named alphabetically with the
radio alphabet
.
WMO World Meteorological Organization replaces IMO under the auspice of the United Nations
.
  • 1953 –
    National Hurricane Center (NOAA)
    creates a system for naming hurricanes using alphabetical lists of women's names.
  • 1954 – First routine real-time numerical weather forecasting. The
    Royal Swedish Air Force
    Weather Service.
– A United States Navy rocket captures a picture of an inland tropical depression near the Texas/Mexico border, which leads to a surprise flood event in New Mexico. This convinces the government to set up a weather satellite program.[40]
NSSP National Severe Storms Project and NHRP National Hurricane Research Projects established. The Miami office of the United States Weather Bureau is designated the main hurricane warning center for the Atlantic Basin.[40]
The first television image of Earth from space from the TIROS-1 weather satellite.
  • 1959 – The first weather satellite, Vanguard 2, was launched on February 17. It was designed to measure cloud cover, but a poor axis of rotation kept it from collecting a notable amount of useful data.
  • 1960 – The first successful weather satellite,
    NOAA have launched since then.[40]
  • 1961 –
    Edward Lorenz accidentally discovers Chaos theory when working on numerical weather prediction
    .
  • 1962 – Keith Browning and Frank Ludlam publish first detailed study of a supercell storm (over Wokingham, UK). Project STORMFURY begins its 10-year project of seeding hurricanes with silver iodide, attempting to weaken the cyclones.[40]
  • 1968 – A hurricane database for Atlantic hurricanes is created for NASA by Charlie Newmann and John Hope, named HURDAT.[40]
  • 1969 –
    Saffir–Simpson Hurricane Scale
    created, used to describe hurricane strength on a category range of 1 to 5. Popularized during Hurricane Gloria of 1985 by media.
ENSO by suggesting that an anomalously warm spot in the eastern Pacific can weaken the east-west temperature difference, causing weakening in the Walker circulation
and trade wind flows, which push warm water to the west.
– The first use of a
General Circulation Model to study the effects of carbon dioxide doubling. Syukuro Manabe and Richard Wetherald at Princeton University
.
Major types: current Stratiform Cirriform Stratocumuliform Cumuliform Cumulonimbiform
Extreme level veils Noctilucent billows or whirls Noctilucent bands
Very high level Nitric acid & water PSC
nacreous PSC
nacreous PSC
High-level Cirrostratus Cirrus Cirrocumulus
Mid-level Altostratus Altocumulus
Low-level Stratus Stratocumulus
fractus
Multi-level or moderate vertical Nimbostratus
Cumulus mediocris
Towering vertical
Cumulus congestus
Cumulonimbus

Major types shown here include the ten tropospheric genera that are detectable (but not always identifiable) by satellite, and several additional major types above the troposphere that were not included with the original modification. The cumulus genus includes four species that indicate vertical size and structure.

– CAMEX3, a NASA experiment run in conjunction with NOAA's Hurricane Field Program collects detailed data sets on Hurricanes Bonnie, Danielle, and Georges.
  • 1999 – Hurricane Floyd induces fright factor in some coastal States and causes a massive evacuation from coastal zones from northern Florida to the Carolinas. It comes ashore in North Carolina and results in nearly 80 dead and $4.5 billion in damages mostly due to extensive flooding.

21st century

See also

References and notes

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External links