World Meteorological Day Ppt

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    WORLD METOEROLOGICAL DAY

    EXHIBITION @ HSV

    23 MARCH 2011

    AL

    B.C.RAJAGOPAL

    TEACHER-GEOGRAPHYCHENNAI

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    What is Meteorology?

    Meteorology is the

    interdisciplinary scientificstudy of the atmosphere thatfocuses on weather processes

    and short term forecasting

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    History of MeteorologyIn 600 BC Thales the first Greek Meteorologist described water cycle made a

    seasonal crop forecast.

    In 400 BC Democritus predicted change in weather.

    In 350 BC Aristotle who wrote Meteorology is considered the founder of

    Meteorology.

    In 250 BC Archimedes study the positive buoyancy that is necessary for the

    formation of clouds.

    In 25 AD Pomponius Mela a Geographer for the Roman Empire, formalizedthe climatic zone system.

    In 80 AD, Wang Chang dispels the chinese myth that rains come from heaven.

    The Greek scientist THEOPHRASTUS compiled a book on weatherforecasting, called the book ofsigns

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    Visual Atmospheric Phenomena

    In 1021 Mr.Ibn al HaythamAtmospheric refractionof light

    Roger Bacon was the first to calculate the angular size of the rainbow

    Theodoric of Freiberg & Kamal al-Din al farisi 1st to give the explanation forthe primary rainbow phenomenon.

    Instrumentsand Classification Scales

    In 1441, King sejongssonPrince Munjong invented Rain Gauge.In 1607, Galileo galiliconstructed the Thermoscope.In 1643, Evangelista Toricelli invents the Mercury Barometer.In 1662, Sir Christopher Wren invented, mechanical, self emptying Rain Gauge.

    In 1960 the first Weather Satellite TIROS-1 was launched.

    AtmosphericComposition Research

    >In 1648, Blaise Pascal rediscovers - atmospheric pressure decreaseswithweight

    >In 1777, Antoine Lavoisier discoversOxygen and developsan explanationfor combustion

    >In 1824, Sadi Carnot analyzes the efficiency of Steam Engine using calorictheory

    Researchinto Cyclone and airflow

    *In 1494 Christopher Columbus writes about Hurricane.*In 1686, EdmundHalley studied Trade Winds & Monsoonsand identifies

    solarheatingas the cause of Atmosphericmotions.*In 1735 George Hadley explained Global Circulation with the study of TradeWinds*In 1743 Benjamin Franklin described that cyclonesmove in acontrary

    manner to the windsat theirperiphery

    Observation Network and Weatherforecasting

    #In 1654 the first weather observing network - by Ferdinando II de medici.#In 1832 Electro MagneticTelegraphcreatedby Baron Schilling.

    #In 1854 United KingdomsMeteorologicaloffice was establishedand in1860 its first weather forecast werepublished in Times Newspaper.# In 1875 India Meteorological Department was established.# In 1881 Finnish Meteorological office was established in HelsinkiUniversity

    Numerical Weather Predictions*In 1922 Lewis Fry Richardson - WeatherPrediction by Numerical Process*In 1950sweather forecast with Barotropicmodelspredict Rossby Waves

    *In 1960s ChaosTheory was mathematically describedby Edward Lorenz.

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    TYPES OFMETEOROLOGY DEALS WITH

    SYNOPTIC METEOROLOGY Day to day analysis and forecasting of weather

    DYNAMIC METEOROLOGYDescribe the atmospheric process through

    mathematical equations

    PHYSICAL METEOROLOGYSolar radiation, absorption and scattering in theearth-atmospheric system, cloud physics and rain

    process

    AGRICULTURALMETEOROLOGY Crop yields and reduction of crop losses

    APPLIED METEOROLOGY

    Design of aircraft, control of air pollution,architectural design, urban planning, exploitation

    of solar and wind energy, air conditioning and

    development of tourism

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    METEOROLOGICAL PHENOMENONAnticyclone, Arctic cyclone, Clouds

    Derecho, Diamond dust,Drought, Dust devil , Dust storm, Foehn wind, Hail,Halo, Hurricane, Ice pellets, Indian summer,

    Lake effect snow, Light pillar, Lightning,

    Mesocyclone, Morning glory cloud,Novaya Zemlya Effect, Rain,Rain and snow mixed, Rainbow,

    Sleet, Snow,

    Subtropical cyclone, Sun dog, Sun shower,Supercell, Temperature inversion, Thunder,

    Thundersnow, Tornado, Tropical storm,

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    WEATHERWeather is a day to day condition

    of a particular place

    CLIMATEThe climate is the common

    weather conditions at a particularplace over a longer period of time.

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    APPLICATIONS

    WEATHER FORECASTING

    AVIATION METEOROLOGY

    AGRICULTURAL METEOROLOGY

    HYDROMETEOROLOGY

    NUCLEAR METEOROLOGY

    MARITIME METEOROLOGY

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    Air Pressure and Humidity

    Air pressure is the weight of theatmosphere pressing down on theearth. It is measured by a barometer inunits called millibars. Most

    barometers use mercury in a glasscolumn, like a thermometer, to

    measure the change in air pressure.

    Relative HumidityRelative humidity is the amount of

    moisture the air can hold before it

    rains. The most it can hold is 100percent. Humidity is measured by aPsychrometer, which indicates theamount of water in the air at any one

    temperature.

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    GABRIEL FAHRENHEITPoland

    May 1686 to Sep 1736

    Fahrenheit Temperature Scale

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    WILLIAM MORRIS DAVISUSA

    Feb 1850 to Feb 1934

    Cycle of Erosion

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    JOHN DALTON England

    Sep 1766 to July 1844

    Law of Partial Pressure

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    ChristophorusHenricus DiedericusBuys BallotNetherlands

    Oct 1817 to Feb 1890

    First chairman of the International

    Meteorological Organization

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    William Ferrel - USA1817 to 1891

    Theories on Mid-latitude AtmosphericCirculation

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    ALFRED WEGENERGermany

    Nov 1880 To Nov 1930

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    Wladimir Koppen - Russia

    Sep 1846 To June 1940

    Koppen Climate Classification System

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    AndersCelsius - Sweden

    Nov 1701 To Apr 1744

    Proposed the CelsiusTemperature scale

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    Aristotle

    Attempted to forecast weather withastrological events

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    Galileo Galilee - ItalyFeb 1564 to Jan 1642

    In about 1593, Galileo constructed a thermometer

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    EvangelistaTorricelliItaly

    Oct 1608 to Oct 1647

    Invented Barometer

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    Sir Christopher Michael Wren

    EnglandOct 1632 to Feb 1723

    Fabricated Weather-Clock for Observations

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    Clement Lindley WraggeEngland

    Sep 1852 Dec 1922

    Started the trend ofusing people's names forCyclones

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    Dmitry LachinovRussia

    1842 to 1902

    Wrote the first book on Meteorology

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    Pavel MolchanovRussia

    Feb 1893 to Oct 1941

    Invented and launched

    Radiosonde

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    Alexander MikhailevichObukhovRussian May 1918 to Dec 1989

    Founder of Modern Boundary Layer of Meteorology

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    Prem Chand Pandey

    IndiaBorn 10/08/1945

    Known for Weather

    Satellite & RemoteSensing SatelliteResearch

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    Pisharoth Rama PisharotyIndia

    Feb 1909 to Sep 2002

    Member of the ScientificAdvisory Board of theWorld Meteorological

    Organization from1963 to 1968

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    JagdishShukla

    India Born 1944

    Member ofJointScientificCommittee

    Of World ClimateResearch Programme

    Of World Meteorological

    Organization.

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    Shen KuoChina 1031 to 1095

    Hypothesized the

    Concept of ClimateChange

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    Edmond HalleyEngland

    Nov 1656 to Jan 1742

    Identified SolarHeating is the cause of

    Atmosphericmotions.First one to put the

    Trade windsandMonsoon on charts

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    FrancisGaltonEngland

    Feb 1822 to Jan 1911Devised first Weather

    Map& Proposed aTheory ofAnticyclone

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    Helmut LandsbergUSA - Feb 1906 to Dec 1985

    Led the field of ClimatologyUsing Statistical Methods.

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    Sydney Chapman

    British 1888 to 1970First IntroducedAeronomy - the

    science of the upperregion of theatmosphere.

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    Both of them discovered the OZONE LAYER in 1913

    HENRI BUISSONCHARLES FABRY

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    Richard Assmann (German Meteorologist) &Lon Teisserenc de Bort(French Meteorologist)

    Discoverers of STRATOSPHERE

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    The President of the Royal Meteorological Society

    PROFESSOR TIM PALMER

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    JON MALAYPresident - American Meteorological Society

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    ALEXANDER BERRITSKIYPRESIDENT - WMO

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    Mitsuhiko Hatori, Director-General of

    the Japan Meteorological Agency

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    PIETERVAN

    MUSSCHENBROEK ATMOMETER

    MEASUREMENT OF EVAPORATION

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    ALTIMETER

    Diagram showingthe face of the"three-pointer"sensitive aircraft

    altimeterdisplaying an

    altitude of 10,180

    feet.

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    HYGROMETER

    is a deviceused for

    measuring the

    HUMIDITY ofthe air

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    ACTINOMETERTo measure the heating power of radiation

    JOHN HERSCHEL -ENGLAND

    1792 TO 1871

    ACTINOMETER

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    CEILOMETERTo determine the height ofacloud base using laser

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    HELIOMETERDesigned for measuring the variation of the

    suns diameter at different seasons.

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    HYPSOMETER

    Instrument used to measure height or altitude

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    MANOMETER PRESSURE MEASURING DEVICE

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    Thehail on Egypt. Hail is a solid form of Precipitation

    THE HAIL

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    The first weather satellite, Vanguard 2,was launched on February 17, 1959

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    GOES-8, a United States weathersatellite launched on October 16, 1975,

    at Florida USA

    f l h ll

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    TIROS - 1 First Successful Weather Satellite

    Date of Launch : 01/04/1960 at Florida, USA

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    RI

    SAT 2 ARadar imageSatellite

    With allWeather

    Capacity totake images

    of the earth.

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    FULMINOLOGY

    The study or science

    of lightning is calledFulminology

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    BRONTOLOGY

    The study or science of

    THUNDER is calledBrontology

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    ACID RAINAcid rain is a rain or any other

    form of precipitation that is

    unusually acidic, i.e. elevatedlevels of hydrogen ions (low pH).Acid Rain was noted in the 17th

    century by John Evelyn.

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    Highest Rainfall @ Cherrapunji Meghalaya 1484m MSL

    25.3 degree N & 91.7 degree EastHolds two Guinness world records for

    1).22,987 millimeters (905.0 in) of rainfall between August 1860 andJuly 1861

    2).9,300 millimeters(370 in) in July 1861

    Why? - Cherrapunji receives rains from the Bay of Bengal arm of the Indian

    summer Monsoon. The monsoon clouds fly unhindered over the plains of Bangladesh for about 400 km. Thereafter, they hit the Khasi Hills which abruptlyrise out of the plains to reach a height of about 1370 m above mean sea levelwithin of 2 to 5 km. The geography of the hills with many deep valleys channelsthe low-flying (150300 m) moisture-laden clouds from a wide area to converge

    over Cherrapunji. The winds push the rain clouds through these gorges and up thesteep slopes. The rapid ascent of the clouds into the upper atmosphere hastensthe cooling and helps vapours to condense. Most of Cherrapunji's rain is the resultof air being lifted as a large body of water vapour. The extremely large amount ofrainfall at Cherrapunji is perhaps the best-known feature of orographic rain innortheast India.

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    Dont run, otherwise the rain may stop

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    RAIN GAUGE or

    UDOMETER orPLUVIOMETER orOMBROMETER to measure

    RAINFALL

    Ancient Greek periodabout 500 BC the firsttime the rainfall was

    recorded.

    DISDROMETER

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    DISDROMETER

    A disdrometer is aninstrument used to

    measure the drop

    size distribution andvelocity of falling

    hydrometeors.Some disdrometers

    can distinguishbetween rain,graupel, and hail.

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    DERECHO

    Violent Windstorm associated with Thunderstorm in Minnesota

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    DIAMOND DUSTGround level Cloudscomposed ofIce Crystals referred asCleary Sky Precipitation

    Most common in Antarcticaand Arctic

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    Dust devil, astrong long-lived whirlwind in Arizona

    DUST DEVIL

    FOEHN WIND

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    FOEHN WIND

    FORMATION OF FOEHN WIND FOEHN CLOUDS IN GENEVA

    FOEHN isa dry down-slope , rain shadow

    wind at the lee of the mountain side

    NOVAYA ZEMLYA EFFECT

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    NOVAYA ZEMLYA EFFECTA polar mirage caused by high refraction of sunlight give the

    impression that the sun is rising earlier than it actually should

    TORNADO

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    TORNADOTornado is a violent, dangerous column of

    air mostly in the form of condensation funnel

    SUN DOG

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    SUN DOGA sun dog also called a mock sun or a phantomsun) is an atmospheric phenomenon that creates

    bright spots of light in the sky, often on a luminousring or halo on either side of the sun.

    H l ( ti l h )

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    Halo (optical phenomenon)

    A man withahalo around him

    A halo isan optical phenomenon produced by ice crystals

    creating colored or white arcsand spotsin the sky

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    SUNLIGHT

    The totalfrequencyspectrum of

    electromagneticradiation givenoff by the Sun

    An ANTICYCLONE is a large-scale circulation of winds

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    An ANTICYCLONE is a large scale circulation of windsaround a central region of high atmospheric pressure,

    clockwise in the Northern Hemisphere, counterclockwise

    in the Southern Hemisphere

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    POLAR CYCLONES

    A polar cyclone is a low pressureweather system usuallyspanning 1,0002,000

    kilometers (6201,240 miles) in

    which the air is circulating in a

    counter-clockwise fashion (in thenorthern hemisphere).

    SLEET refers to two distinct forms of precipitation

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    SLEET refers to two distinct forms of precipitation:Rain and snow mixed, snow that partially melts as it falls.Ice pellets, one of three forms of precipitation in a US-style

    Wintry Mix", the other two being snow and freezing rain.

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    A LIGHT PILLARis a visual phenomenon

    created by the reflectionof light from ice crystals

    with near horizontalparallel planar surfaces.

    The light can come fromthe sun (usually at or lowto the horizon) in whichcase the phenomenon is

    called a sun pillar or solarpillar. It can also comefrom the moon or from

    terrestrial sources such asstreetlights.

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    A MESOCYCLONEis a vortex of air,

    approximately 2 to 10 miles indiameter (the mesoscale of

    meteorology), within a

    convective storm. That is, it is airthat rises and rotates around a

    vertical axis, usually in the samedirection as low pressure systems

    in a given hemisphere.

    MESOCYCLONE

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    MESOCYCLONE

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    S.No ABBREVIATIONS

    1 ACYC ANTICYCLONE

    2 BRM BAROMETER

    3 CLD CLOUD

    4 DRZL DRIZZLE

    5 E ENDING OF PRECIPITATION (IN MINUTE-METAR)

    6 FAH FAHRENHEIT

    7 GV GROUND VISIBILITY

    8 HIXAT HIGHEST TEMPERATURE EXCEEDED FOR ALL TIME