41. Coriolis Physics Faces. Gaspard gustave de coriolis (17921843). “coriolisentered the Ecole Polytechnique in 1808. After graduation he served http://faculty.rmwc.edu/tmichalik/coriolis.htm

Physics Faces Gaspard Gustave de Coriolis “Coriolis entered the Ecole Polytechnique in 1808. After graduation he served for several years in the corps of engineers (of the Ponts et Chausees). In 1816 he started his teaching career. He was an attentive, effective and solicitous teacher. He was also a bachelor and invalid. As a result of studying formulations of dynamical problems in rotating machinery he was led to consider the effect of changes of coordinate systems in analytical mechanics. The result of these studies was presented to the Academie des Sciences on June 6, 1831. A French oceanographic vessel was named after hin in 1963.” From: An Introduction to the Coriolis Force by H. Stommel and D. Moore, Columbia Univ. Press, 1989.

42. Gaspard-Gustave Coriolis - Wikipedia Gaspardgustave coriolis. Gaspard-gustave de coriolis (urodzony 21 maja1792 - zmarl 19 wrzesnia 1843), francuski fizyk i matematyk. http://pl.wikipedia.org/wiki/Gaspard-Gustave_Coriolis

Gaspard-Gustave Coriolis Z Wikipedii, wolnej encyklopedii. Gaspard-Gustave de Coriolis (urodzony 21 maja - zmarł 19 września francuski fizyk i matematyk. Był zastępcÄ profesora matematyki w ‰cole Polytechnique w Paryżu ). Badał prawa ruch³w, zwłaszcza ruch³w na powierzchni ziemi. Zobacz: efekt Coriolisa To jest tylko zalÄ Å¼ek artykułu . Jeśli możesz, rozbuduj go. Views artykuł dyskusja edytuj historia Personal tools Logowanie nawigacja Strona gł³wna Ostatnie zmiany Losuj stronę Pomoc ... Dary pieniężne Szukaj narzędzia LinkujÄ ce Zmiany w dolinkowanych Strony specjalne W innych językach English Tę stronę ostatnio zmodyfikowano o 17:30, 11 mar 2004 Treść udostępniana na licencji GNU Free Documentation License O Wikipedii Informacje prawne

43. HighBeam Research: ELibrary Search: Results 1998. All rights reserved. 12. coriolis, Gaspard gustave de (17921843)The Hutchinson Dictionary of Scientific Biography; January 1, 1998 http://www.highbeam.com/library/search.asp?FN=AO&refid=ency_refd&search_dictiona

44. HighBeam Research: Search Results: Article coriolis, Gaspard gustave de (17921843). The Hutchinson Dictionaryof Scientific Biography; 1/1/1998. Read the Full Article, Get http://www.highbeam.com/library/doc0.asp?DOCID=1P1:28910325&num=7&ctrlInfo=Round

45. Glossary hyperbola. Coordinated Universal Time (UTC) Universal Time (whichsee). coriolis, Gaspard gustave de 17921843. French engineer http://cseligman.com/text/appendix/glossary.htm

Glossary (Work in progress) A B C D ... N - Z A aberration One of a number of optical distortions produced by an optical instrument, caused not by a defect in the instrument, but by the nature of its design, and the laws of optical physics. absolute magnitude A number specifying the brightness that a star would have if viewed from a distance of 10 parsecs. Because this is a fixed distance, it is a measure of the star's intrinsic, or actual, brightness. Also see, Apparent Magnitude. absorption Lines Dark lines in the spectrum of an object, caused by the absorption of light by gases lying between us and that object. In the case of a star, the gases may be in the atmosphere, or at the surface of the star, in which case they reveal the physical conditions in those regions. Also see, Interstellar Absorption Lines. achromat A lens made of two pieces of glass (or, occasionally, other materials) with differing optical properties, specifically chosen to minimize chromatic aberration (which see). accretion A process of growth in which small things become large things, through collisions. In the planetesimal accretion theory, the earliest stages of this process involve random collisions, while the later stages involve random collisions aided by gravitational attraction.

46. Gerader Weg Erscheint Erdgebunden Gewunden Translate this page Südhalbkugel scheinbar nach links). Diese Ablenkungskraft ist nachGaspard gustave de coriolis benannt. Mathematisch wird dies so http://www.3sat.de/nano/cstuecke/66066/

Gerader Weg erscheint erdgebunden gewunden Die Frage "Warum drehen sich Luftdruck-Gebiete und abfließendes Wasser in eine bestimmte Richtung?" Volker Franke, Rückersdorf; Werber Kubach, La Eliana-Valencia u.a.) "Luft steigt, Luft fällt" "Günstige Winde für den Orkan" Die Corioliskraft steckt dahinter, wie Hoch- sowie Tiefdruckgebiete sich drehen und wie das Wasser auf Süd- und Nordhalbkugen in den Abfluss kommt - in Rotation. mit: C: Corioliskraft m: Masse des Teilchens v: Geschwindigkeit des Teilchens nano online / mp 3sat.online ist nicht verantwortlich für den Inhalt externer Links

47. How Do We Understand The Coriolis Force? The coriolis force, named after French mathematician Gaspard gustave de coriolis(1792–1843), has traditionally been derived as a matter of coordinate http://ams.allenpress.com/amsonline/?request=get-abstract&issn=1520-0477&volume=

48. Coriolis Gaspard gustave de coriolis 1792 1843. gustave de coriolis wasborn May 21, 1792 in Paris, France and died September 19, 1843. http://www.geomatics.ucalgary.ca/~sneeuw/hall_of_fame/seiten_e/coriolis.html

Gaspard Gustave de Coriolis 1792 - 1843 Gustave de Coriolis was born May 21, 1792 in Paris, France and died September 19, 1843. He is best remembered for his discovery of the Coriolis force relating to centrifugal motion. In a rotating frame of reference, he found a force that was perpendicular both to the flow direction and to the axis of rotation. He revealed how the laws of motion could be used in this rotating frame of reference if an extra force, called the Coriolis acceleration, was added to the equations of motion. Coriolis also developed relationships for the work and kinetic energy involved in the movements of solid bodies.

49. Offline Seznam Personálních Autorit - Coriolis, Gaspard Gustave De 1792 - 1843 coriolis, Gaspard gustave de 1792 1843 Záhlaví, Název, Signatura.ŠTOLL, Ivan, Podivuhodné prírodní úkazy, K 9287. © Mestská http://www.mlp.cz/cz/offline/perlie/c/2027825.htm

Coriolis, Gaspard Gustave de 1792 - 1843 Záhlaví Název Signatura ŠTOLL, Ivan Podivuhodné pøírodní úkazy K 9287 Offline poslední zmìny: 13.10.2003 kont@kt

50. Experiment Corioliskraft Translate this page corioliskraft Versuchsbeschreibung Die corioliskraft wurde nachihrem Entdecker Caspard-gustave de coriolis benannt. Auf einen http://www.fh-merseburg.de/~wwwfpll/lehrmittel/experimente/corioliskraft.htm

Corioliskraft Versuchsbeschreibung: Die Corioliskraft wurde nach ihrem Entdecker Caspard-Gustave de Coriolis benannt. Auf einen Körper, der sich in einem rotierenden Bezugssystem bewegt, wirkt sie senkrecht zur Bewegungsrichtung des Körpers und senkrecht zur Rotationsachse des Systems. Ihr Auftreten wird durch die Trägheit der sich bewegenden Massen verursacht. Bild 1: Versuchsaufbau zum experimentellen Nachweis der Corioliskraft Bedeutung der Corioliskraft: Obwohl die Wirkung der Corioliskraft auf Körper, die sich im rotierenden System "Erde" befinden, vergleichsweise schwach ist, tritt ihre Präsenz auch im alltäglichen Leben immer wieder in Erscheinung. Wer nicht hat sich schon nach einem ausgiebigen Bad gefragt, warum sich der beim Abfließen des Wassers bildende Wirbel immer rechtsherum (nördliche Halbkugel) bzw. linksherum (südliche Halbkugel) dreht. Und welcher Mechanismus führt zur Bildung der mitunter gigantischen Luftmassenwirbel, die wir täglich auf den Satellitenkarten des Wetterberichtes sehen können? Die Antwort findet sich in der Wirkung der Corioliskraft. Wie der Beobachter, der im Experiment auf der rotierenden Scheibe eine scheinbar gekrümmte Bahn der rollenden Kugel wahrnimmt, beobachten wir auf der Erde, wie sich strömende Luft- und Wassermassen aufgrund ihrer Trägheit gleichermaßen auf gekrümmten Bahnen bewegen. Die animierte Grafik auf der linken Seite veranschaulicht diesen Effekt. Auch unter technischen Gesichtspunkten muß die Wirkung der Corioliskraft mitunter berücksichtigt werden. So müssen Flugzeuge, die sich in nördliche oder südliche Richtung bewegen, kurskorregiert werden, damit sie nicht gegenüber der sich drehenden Erde "zurückbleiben". In Nord-Süd Richtung verlaufende Flüsse werden in der nördlichen Hemisphäre auf der rechten Seite, in der südlichen Hemisphäre auf der linken Seite stärker ausgespült. In gleicher Weise läßt sich feststellen, daß bei Eisenbahnstrecken in Nord-Süd Richtung auf der Nordhalbkugel die rechte Schiene und auf der Südhalbkugel die linke Schiene stärker abgenutzt wird.

51. ThinkQuest : Library : Wind, The Invisible Force Dit wordt veroorzaakt dppr de draaiing van de aarde en wordt de coriolis krachtgenoemd, naar de Fransman gustaveGaspard de coriolis (1792-1843), die het http://library.thinkquest.org/C001472/nl/development/coriolis.content.html

Index Earth Science Weather Wind, the invisible force Wind: the invisible force is divided into three main-topics, Development, Hurricanes and Tornadoes. They are supported by the three topics Terms, Interactive and About. In the development section, the user will be informed by the plain way how wind works, how the different forces combined together make the wind that blows right now. In the hurricane section we'll dive furder in the theory of wind. You'll get there an explanation about how a hurricane works, using the forces you learned in the development section. Ofcourse, there are also some "fun"-topics with less educational information, but more interesting to read. The Tornado section is build the same way. Visit Site 2000 ThinkQuest Internet Challenge Languages Dutch Students Sjoerd Sg. St. Canisius, Almelo, Netherlands Hugo Sg. St. Canisius, Almelo, Netherlands Tom Sg. St. Canisius, Albergen, Netherlands Coaches C.M. Sg. St. Canisius, Utrecht, Netherlands Jos Sg. St. Canisius, Vasse, Netherlands Want to build a ThinkQuest site?

52. ThinkQuest : Library : Wind, The Invisible Force This phenomenon is caused by the rotation of the earth and is called the coriolisforce, after the Frenchman gustaveGaspard de coriolis (1792-1843) who http://library.thinkquest.org/C001472/en/development/coriolis.content.html

Index Earth Science Weather Wind, the invisible force Wind: the invisible force is divided into three main-topics, Development, Hurricanes and Tornadoes. They are supported by the three topics Terms, Interactive and About. In the development section, the user will be informed by the plain way how wind works, how the different forces combined together make the wind that blows right now. In the hurricane section we'll dive furder in the theory of wind. You'll get there an explanation about how a hurricane works, using the forces you learned in the development section. Ofcourse, there are also some "fun"-topics with less educational information, but more interesting to read. The Tornado section is build the same way. Visit Site 2000 ThinkQuest Internet Challenge Languages Dutch Students Sjoerd Sg. St. Canisius, Almelo, Netherlands Hugo Sg. St. Canisius, Almelo, Netherlands Tom Sg. St. Canisius, Albergen, Netherlands Coaches C.M. Sg. St. Canisius, Utrecht, Netherlands Jos Sg. St. Canisius, Vasse, Netherlands Want to build a ThinkQuest site?

53. Neue Seite 1 Translate this page de coriolis, gustave (1792 - 1843). Cosserat, Eugene Maurice (1866 - 1931). decoriolis, gustave (1792 - 1843). de Coulomb, Charles (1736 - 1806). dedekind,. http://www.mathe-ecke.de/mathematiker.htm

Abbe, Ernst (1840 - 1909) Abel, Niels Henrik (5.8.1802 - 6.4.1829) Abraham bar Hiyya (1070 - 1130) Abraham, Max (1875 - 1922) Abu Kamil, Shuja (um 850 - um 930) Abu'l-Wafa al'Buzjani (940 - 998) Ackermann, Wilhelm (1896 - 1962) Adams, John Couch (5.6.1819 - 21.1.1892) Adams, John Frank (5.11.1930 - 7.1.1989) Adelard von Bath (1075 - 1160) Adler, August (1863 - 1923) Adrain, Robert (1775 - 1843) Aepinus, Franz Ulrich Theodosius (13.12.1724 - 10.8.1802) Agnesi, Maria (1718 - 1799) Ahlfors, Lars (1907 - 1996) Ahmed ibn Yusuf (835 - 912) Ahmes (um 1680 - um 1620 v. Chr.) Aida Yasuaki (1747 - 1817) Aiken, Howard Hathaway (1900 - 1973) Airy, George Biddell (27.7.1801 - 2.1.1892) Aithoff, David (1854 - 1934) Aitken, Alexander (1895 - 1967) Ajima, Chokuyen (1732 - 1798) Akhiezer, Naum Il'ich (1901 - 1980) al'Battani, Abu Allah (um 850 - 929) al'Biruni, Abu Arrayhan (973 - 1048) al'Chaijami (? - 1123) al'Haitam, Abu Ali (965 - 1039) al'Kashi, Ghiyath (1390 - 1450) al'Khwarizmi, Abu Abd-Allah ibn Musa (um 790 - um 850) Albanese, Giacomo (1890 - 1948) Albert von Sachsen (1316 - 8.7.1390)

54. Biography-center - Letter D de Carlo, Yvonne www.cyranos.ch/munste.htm; de coriolis, gustave www-history.mcs.st-and.ac.uk/~history/Mathematicians/coriolis.html; http://www.biography-center.com/d.html

Visit a random biography ! Any language Arabic Bulgarian Catalan Chinese (Simplified) Chinese (Traditional) Croatian Czech Danish Dutch English Estonian Finnish French German Greek Hebrew Hungarian Icelandic Indonesian Italian Japanese Korean Latvian Lithuanian Norwegian Polish Portuguese Romanian Russian Serbian Slovak Slovenian Spanish Swedish Turkish D 492 biographies www-history.mcs.st-and.ac.uk/~history/Mathematicians/Durer.html D'Alema, Massimo www.uwgb.edu/galta/333/BIOS98/DALEMA.HTM d'Alembert, Jean www-history.mcs.st-and.ac.uk/~history/Mathematicians/D'Alembert.html d'Alembert, Jean-le-Rond www.treasure-troves.com/bios/dAlembert.html D'Inzeo, Raimondo www.olympic.org/uk/athletes/heroes/bio_uk.asp?PAR_I_ID=25085 Da Costa, Jacob Mendez www.whonamedit.com/doctor.cfm/2452.html Da Vinci, Leonardo www.ibiblio.org/wm/paint/auth/vinci/ Da Vinci, Leonardo www.kfki.hu/~arthp/bio/l/leonardo/biograph.html Dadd, Richard www.getty.edu/art/collections/bio/a281-1.html Daddi, Bernardo www.kfki.hu/~arthp/bio/d/daddi/biograph.html Daddi, Bernardo www.getty.edu/art/collections/bio/a1085-1.html Dae-jung, Kim

55. Gustave-Gaspard Coriolis --  Encyclopædia Britannica Cite this article. gustaveGaspard coriolis. born May 21, 1792, Paris MLA style " gustave-Gaspard coriolis." Encyclopædia Britannica. 2004 http://www.britannica.com/eb/article?eu=26729

56. Coriolis Effect coriolis Effect coriolis effect is an inertial force described by the 19thcentury French engineer-mathematician gustave-Gaspard coriolis in 1835. http://zebu.uoregon.edu/~js/glossary/coriolis_effect.html

Coriolis Effect Coriolis effect is an inertial force described by the 19th-century French engineer-mathematician Gustave-Gaspard Coriolis in 1835. Coriolis showed that, if the ordinary Newtonian laws of motion of bodies are to be used in a rotating frame of reference, an inertial forceacting to the right of the direction of body motion for counterclockwise rotation of the reference frame or to the left for clockwise rotationmust be included in the equations of motion. The effect of the Coriolis force is an apparent deflection of the path of an object that moves within a rotating coordinate system. The object does not actually deviate from its path, but it appears to do so because of the motion of the coordinate system. The Coriolis deflection is therefore related to the motion of the object, the motion of the Earth, and the latitude. For this reason, the magnitude of the effect is given by 2 sin , in which is the velocity of the object, is the angular velocity of the Earth, and is the latitude. The Coriolis effect has great significance in astrophysics and stellar dynamics, in which it is a controlling factor in the directions of rotation of sunspots. It is also significant in the earth sciences, especially meteorology, physical geology, and oceanography, in that the Earth is a rotating frame of reference, and motions over the surface of the Earth are subject to acceleration from the force indicated. Thus, the Coriolis force figures prominently in studies of the dynamics of the atmosphere, in which it affects prevailing winds and the rotation of storms, and in the hydrosphere, in which it affects the rotation of the oceanic currents.

57. Gaspard-Gustave Coriolis - Wikipedia, The Free Encyclopedia Gaspardgustave coriolis. He is sometimes referred to as gustave-Gaspard coriolis,gustave coriolis and variations thereof. link title. Headline text. http://en.wikipedia.org/wiki/Gaspard-Gustave_Coriolis

Gaspard-Gustave Coriolis From Wikipedia, the free encyclopedia. Gaspard-Gustave de Coriolis May 21 September 19 French engineer and scientist . His interest in the dynamics of rotating machines led him to derive the differential equations of motion from the point of view of a coordinate system which is itself rotating, which he first presented in to the Académie des Sciences. Due to the importance of this work, the Coriolis effect is named for him. He is sometimes referred to as Gustave-Gaspard Coriolis Gustave Coriolis and variations thereof. Views Article Discussion Edit History Personal tools Log in Navigation Main Page Community portal Current events Recent changes ... Donations Search Toolbox What links here Related changes Special pages Other languages Polski This page was last modified 04:19, 30 May 2004. All text is available under the terms of the GNU Free Documentation License (see for details). About Wikipedia

58. Coriolis Effect - Wikipedia, The Free Encyclopedia encyclopedia. In physics, the coriolis effect is an inertial force firstdescribed by Gaspardgustave coriolis, a French scientist, in 1835. http://en.wikipedia.org/wiki/Coriolis_effect

Coriolis effect From Wikipedia, the free encyclopedia. In physics , the Coriolis effect is an inertial force first described by Gaspard-Gustave Coriolis , a French scientist, in . When the equations of motion are formulated in a rotating coordinate system a term arises which looks like a force, called the Coriolis force . See also centrifugal force In changing from an essentially inertial coordinate system (such as the "frame of the fixed stars") to a rotating frame of reference (such as Earth), a term appears in the equation of motion described by the formula: where bold indicates vector quantities, m is mass v is the velocity and is the angular velocity of the coordinate system. Note that this equation ignores the second-order term in , which in geophysical terms is small, and can anyway be absorbed into the gravitational potential term. Hurricane Isabel east of the Bahamas on 2003-09-15. Photograph courtesy NASA. This equation means that the force will be proportional to the velocity of the object and the rotation of the coordinate system. The force will be in a direction perpendicular to the velocity (and thus does no work). If an object is travelling on earth in the northern hemisphere, the Coriolis force will deflect the object to the right. In the southern hemisphere the reverse is true, while at the equator the horizontal component of the force is zero for horizontal motions. For instance, the effect breaks up the atmospheric circulation from the tropics to the polar regions into a series of cells in which the surface winds have a prevailing eastward or westward component.

59. Gaspard-Gustave Coriolis Gaspardgustave coriolis. He is sometimes referred to as gustave-Gaspard coriolis,gustave coriolis and variations thereof. This article is from Wikipedia. http://www.fact-index.com/g/ga/gaspard_gustave_coriolis.html

Main Page See live article Alphabetical index Gaspard-Gustave Coriolis Gaspard-Gustave de Coriolis French engineer and scientist . His interest in the dynamics of rotating machines led him to derive the differential equations of motion from the point of view of a coordinate system which is itself rotating, which he first presented in to the Académie des Sciences. Due to the importance of this work, the Coriolis effect is named for him. He is sometimes referred to as Gustave-Gaspard Coriolis Gustave Coriolis and variations thereof. This article is from Wikipedia . All text is available under the terms of the GNU Free Documentation License

60. Coriolis Effect coriolis effect. The coriolis effect is an inertial force first describedby Gaspardgustave coriolis, a French scientist, in 1835. http://www.fact-index.com/c/co/coriolis_effect.html

Main Page See live article Alphabetical index Coriolis effect The Coriolis effect is an inertial force first described by Gaspard-Gustave Coriolis , a French scientist, in . When an object is moving in a rotating coordinate system, the path of the object appears to deviate due to the Coriolis effect. If you are in the moving coordinate system, this deviation makes it look like a force is acting upon the object (due to Newton's laws of motion ), but actually there is no real force acting on the object, the effect is due to rotation (associated with an acceleration ) of the coordinate system itself. A similar effect from a moving frame of reference is the centrifugal force In a rotating frame of reference (such as the earth), the apparent force can be described by the formula: where bold indicates vector quantities, m is mass v is the velocity and is the angular velocity of the coordinate system. This equation means that the force will be proportional to the velocity of the object and the rotation of the coordinate system. The force will be in a direction perpendicular to the velocity. If an object is travelling on earth in the northern hemisphere, the Coriolis force will deflect the object to the right. In the southern hemisphere the reverse is true, while at the equator the horizontal component of the force is zero for horizontal motions. The Coriolis force plays a strong role in weather patterns, where it affects prevailing

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